HIGHLIGHTS
- Novo has advanced Pilbara high-grade gold and gold-antimony prospects which will be the focus for exploration and drilling in H2 2025.
- Exploration at the Sherlock Crossing Au-Sb prospect has defined a coherent 1.5 km antimony in soil anomaly (at > 15 ppm Sb), with gold anomalism up to 85 ppb Au, with all heritage and compliance approvals now in place for exploration drilling.
- At the Southeast Wyloo Au-Sb-Ag-Cu Project, plans are in place to complete mapping and rock chip sampling in preparation for drill program planning.
- Heritage access approval has been obtained for low-impact exploration work at the Teichman gold prospect in the northern Egina Gold Camp, within the Yandeyarra Reserve. High-grade gold has been defined during historic rock sampling programs in the area.
- Results from reconnaisance aircore (AC) drilling at Balla Balla delineated broad zones of low-level gold anomalism (peak 0.114 ppm Au) along the Sholl Shear. Significant results from multielement assays of bottom hole samples and select drill holes include 96.8 ppm Ag, 182 ppm Sb, 353 ppm Cu, and 71.6 ppm Bi.
- Northern Star Resources Limited (ASX: NST), Novo’s new partner in the Egina Farm-in/Joint Venture arrangement (following its acquisition of De Grey Mining) has commenced reviewing previous data in planning for future exploration programs.
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Commenting on the Company’s Pilbara exploration activity, Mike Spreadborough, Executive Co-Chairman and Acting Chief Executive Officer, said “We have been methodical in our assessment of advanced gold and antimony targets over the first half of 2025, which has set Novo up for a busy second half of exploration.
“We have identified several compelling targets including the Sherlock Crossing prospect, where our highly experienced geological team has defined a 1.5km antimony anomaly, which we will be a priority for drilling in the short term.
Importantly, the price of gold continues to strengthen and global interest in antimony continues to grow rapidly, which places Novo in an exciting position as we execute on these programs and complete drilling over the coming months.
“Furthermore, Novo is pleased that Northern Star Resources, Novo’s new partner in the Egina Farm-in and Joint Venture arrangement (following the completion of its acquisition of De Grey Mining), has commenced reviewing key data for future exploration work. The Egina JV area covers a large and strategic land position in the prospective Mallina Basin and importantly, the Egina Gold Project tenements are highly prospective for significant intrusion related deposits and share similar attributes to the nearby Hemi deposit.”
PERTH, Western Australia, June 19, 2025 (GLOBE NEWSWIRE) -- Novo Resources Corp. (Novo or the Company) (ASX: NVO) (TSX: NVO) (OTCQX: NSRPF) is pleased to provide an update on its Pilbara-wide exploration completed during H1 2025, including the Balla Balla Gold Project AC drill program. In the Pilbara the focus for the second half will be on high-grade gold and gold-antimony exploration projects.
Novo has also been actively exploring its New South Wales projects, undertaking RC drilling at the Tibooburra Gold Project (results pending) and preparation work, including mapping and geochemical sampling, at the John Bull Gold Project. Drilling is expected to commence at John Bull in early Q3 2025 (weather and access approval permitting).

Figure 1: Novo Tenure showing the Egina Gold Camp, Balla Balla Gold Project, and gold prospects.
PILBARA EXPLORATION PORTFOLIO
Balla Balla Gold Project
Balla Balla is an early-stage exploration project centred on the Sholl Shear Zone (Figure 1)1. In April 2025, Novo completed a maiden AC program testing several prospects over a 10 km trend, targeting the Sholl Shear Zone and interpreted splay faults under shallow cover.
A total of 187 AC holes for 5,996 m were completed on regionally spaced lines varying from 640 m to 2.8 km apart (Figure 2). Hole depths range from 5 m to 79 m with cover varying between 5 m to 35 m depth (average 22 m). Samples were collected as 3 m composites for the entire hole and assayed for gold using fire-assay, and a bottom of hole (BOH) sample was taken and assayed for gold and a 52-multielement suite using fire assay and four-acid digest. Seven holes have been selected with intense sulphide mineralisation, quartz veining or strong alteration for multi-element assaying with results from two holes pending.

Figure 2: AC collar locations on interpreted regional geology and structure
Peak results from broad zones of low-level anomalism associated with the Sholl Shear includes 114 ppb Au (Figure 3). However, numerous additional anomalies have been defined by BOH and select hole multielement assay. These include:
- 1 m @ 96.8 ppm Ag and 8.1 ppm Sb from 28 m in YUA0113 (BOH sample)
- 1 m @ 182 ppm Sb and 6.72 ppm Ag from 44 m in YUA0054 (BOH sample – multielement assay results for entire hole pending)
- Anomalous Bi, Sb and Te from 57 m to 78 m in YUA0161, with peak results of 71.6 ppm Bi, 47.3 ppm Sb, and 6.23 ppm Te (multielement assay for entire hole)
- Anomalous Mo, Sb, Au, Te from 45 m to 74 m in YUA0162, with peak results of 70 ppb Au, 14.50 ppm Bi, 99.7 ppm Mo, 11.0 ppm Sb and 11.8 ppm Te (multielement assay for entire hole)
- 1 m @ 299 ppm Cu and 24.7 ppm Sb from 43 m in YUA0182 (BOH sample)
- 12 m @ 277 ppm Cu, 303 ppm Zn and 11.5 ppm Sb from 30 m in YUA0185 (multielement assay for entire hole)
Refer to Appendix 1 for collar details and peak gold results. Refer to Appendix 2 for end of hole and downhole multielement assays.
Peak Au-Ag-Bi-Sb-Cu-Mo is present at Ramquarry and south Babbage along the Sholl Shear and are related to sub-massive pyrite mineralisation, strong silica-chlorite alteration an/or zones of intense quartz veining, indicating significant hydrothermal activity. Peak silver values are related to an interpreted fold axis in regional magnetics and porphyritic mafic intrusion.
Further work, once all results are returned, will include assaying full holes for the multielement assay suite in anomalous areas, spectral imaging on selected intervals to determine alteration mineralogy and rock composition, and petrology on selected samples. After the full results are returned and interpreted along with other high-level studies, follow-up and extensional drilling will be planned if warranted.

Figure 3: AC collar locations over regional geological interpretation and airborne magnetics, showing maximum downhole gold values
Sherlock Crossing
Novo completed a soil sampling program to extend coverage of an antimony in soil anomaly and high order stream sediment anomaly, to the southwest of the Sherlock Crossing historic workings area (Figure 4). Samples were collected on a 40 m x 80 m grid.
Results define a strong and coherent antimony anomaly extending over 1.5 km in strike length, and a width of 200 m. Peak soil sample results include 85 ppb Au and 48.3 ppm Sb (Figure 4). Anomalous antimony occurs in a strongly altered and sheared ultramafic unit which sporadically outcrops over 2.3 km strike, trending under colluvial cover to the south. Rock samples from the highly sheared and altered ultramafic, returned results of up to 0.22% Sb without significant quartz veining.
Refer to Appendix 3 for all soil sample results, and Appendix 4 for all rock sample results.
All heritage and compliance approvals have been obtained to enable a maiden RC drilling program adjacent to the historical Sherlock Crossing workings to test promising gold and antimony mineralisation, where targeted rock chip sampling yielded grades of up to 4.7% Sb and 146.7 g/t Au2.
Drilling is planned for H2 2025. Meanwhile, detailed mapping and sampling will continue to assist in targeting the core of the soil anomaly to the southwest.

Figure 4: Sherlock Crossing, showing extended soil anomaly > 15 ppm Sb to the SW of the proposed first pass drilling area at the Clarke Mine2
Egina Gold Camp – Egina Earn-in/JV (Northern Star earning a 50% interest)
Northern Star Resources Limited (ASX: NST) recently finalised its acquisition of De Grey Mining (ASX: DEG). The NST group has commenced reviewing previous data in planning for future exploration programs in the Becher and surrounding area.
In June 2023, Novo entered into an earn-in and joint venture agreement with De Grey for the Company’s Becher Projectand adjacent tenements within the Egina Gold Camp. De Grey exceeded the A$7 million minimum expenditure commitment under the earn-in in September 2024 and is required to spend a further A$18 million by June 30, 2027, to earn a 50% interest in the Becher Project at which time an unincorporated joint venture would be established.3
Egina is located near the 13.6 Moz Hemi Gold Project4. No assurance can be given that a similar (or any) commercially viable mineral deposit will be determined at Novo’s Egina Project.
Egina Gold Camp - Tabba Tabba Shear Corridor
Exploration of the Tabba Tabba Shear Corridor, part of Novo’s Egina Gold Camp, progressed in 2024, with first pass surface geochemistry and mapping now covering the central part of the Corridor. Novo has prioritised obtaining access to the Teichman prospect (Figure 5), located within the Yandeyarra Reserve5, where previous explorers obtained high-grade surface results from several prospects over 2.3 km strike, including 25.5 g/t Au and 32.3 g/t Au from rock samples6.
Approval to carry out low-impact exploration activities on parts of Novo’s tenements within the Yandeyarra Aboriginal Reserve has now been achieved. The proposed work will comprise up to ten days of mapping and targeted rock sampling. Only limited modern exploration has been undertaken in the Yandeyarra Reserve.

Figure 5: Main prospects of the Tabba Tabba Shear Corridor
Southeast Wyloo
During H2 2024, Novo completed a review of the Sb-Au potential across its Pilbara ground holding. In addition to Sherlock Crossing, Southeast Wyloo was also ranked highly for antimony potential and includes two, 2 km-strike high-order antimony (± gold) stream sediment anomalies, where reconnaissance rock chip sampling completed in mid-2023 yielded peak results of 387 g/t Ag, 2.4% Cu, 0.38%, and 0.52 g/t Au, 5.0% Pb and 1.6% Zn7.
Plans are in place to complete mapping and rock chip sampling during H2 2025 in preparation for drill program planning.
Authorised for release by the Board of Directors.
CONTACT
Investors: Mike Spreadborough +61 8 6400 6100 info@novoresources.com | North American Queries: Leo Karabelas +1 416 543 3120 leo@novoresources.com | Media: Cameron Gilenko +61 466 984 953 cameron.gilenko@sodali.com |
QP STATEMENT
Mrs. Karen (Kas) De Luca (MAIG), is the qualified person, as defined under National Instrument 43-101 Standards of Disclosure for Mineral Projects, responsible for, and having reviewed and approved, the technical information contained in this news release. Mrs De Luca is Novo’s General Manager Exploration.
JORC COMPLIANCE STATEMENT
New Exploration Results
The information in this news release that relates to exploration results at Novo’s Pilbara tenure is based on information compiled by Mrs De Luca, who is a full-time employee of Novo Resources Corp. Mrs De Luca is a Competent Person who is a member of the Australian Institute of Geoscientists. Mrs De Luca has sufficient experience that is relevant to the style of mineralisation and the type of deposits under consideration and to the activity being undertaken to qualify as a Competent Person as defined in the 2012 Edition of the 'Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves'. Mrs De Luca consents to the inclusion in the report of the matters based on her information in the form and context in which it appears.
Previous Exploration Results
The information in this news release that relates to previously reported exploration results at Novo’s Pilbara tenure is extracted from:
a) | Novo’s ASX announcement entitled Pilbara Exploration Update released to ASX on 10 December 2024; |
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b) | Novo’s ASX announcement entitled Nunyerry North High-Grade Gold Zone Extended released to ASX on 30 August 2024; and |
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c) | Novo’s ASX announcement entitled Evaluation of Pilbara Antimony-Gold Potential Generates Positive Results released to ASX on 12 September 2024, |
each of which is available to view at www.asx.com.au. The Company confirms that it is not aware of any new information or data that materially affects the information included in the original market announcements and that all material assumptions and technical parameters underpinning the estimates in the market announcements continue to apply and have not materially changed. The Company confirms that the form and context in which the competent persons findings are presented have not been materially modified from the original market announcements.
FORWARD-LOOKING STATEMENTS
Some statements in this news release may contain “forward-looking statements” within the meaning of Canadian and Australian securities law and regulations. In this news release, such statements include but are not limited to planned exploration activities and the timing of such. These statements address future events and conditions and, as such, involve known and unknown risks, uncertainties and other factors which may cause the actual results, performance or achievements to be materially different from any future results, performance or achievements expressed or implied by the statements. Such factors include, without limitation, customary risks of the resource industry and the risk factors identified in Novo’s annual information form for the year ended December 31, 2024 (which is available under Novo’s profile on SEDAR+ at www.sedarplus.ca and at www.asx.com.au) in the Company’s prospectus dated 2 August 2023 which is available at www.asx.com.au. Forward-looking statements speak only as of the date those statements are made. Except as required by applicable law, Novo assumes no obligation to update or to publicly announce the results of any change to any forward-looking statement contained or incorporated by reference herein to reflect actual results, future events or developments, changes in assumptions or changes in other factors affecting the forward-looking statements. If Novo updates any forward-looking statement(s), no inference should be drawn that the Company will make additional updates with respect to those or other forward-looking statements.
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1 Refer to Novo’s ASX announcement dated 20 March 2025 - Aircore drilling to commence at Balla Balla.
2 Refer to Novo’s ASX announcement dated 10 December 2024 - Pilbara Exploration Update
3 Refer to Novo’s ASX announcement dated 10 October 2024 – De Grey reaches minimum spend at Novo’s Egina Gold Project
4 Refer to De Grey’s ASX Announcement, Hemi Gold Project mineral Resource Estimate (MRE) 2024, dated 14 November 2024
5 Refer to Novo’s ASX announcement dated 10 December 2024 - Pilbara Exploration Update
6 Refer to Novo’s ASX announcement dated 30 August 2024 – Nunyerry North High-Grade Gold Zone extended and Egina Gold Camp exploration targets advanced
7 Refer to Novo’s ASX announcement dated 12 September 2024 – Evaluation of Pilbara Antimony-Gold Potential Generates Positive Results
ABOUT NOVO
Novo is an Australian based gold explorer listed on the ASX and the TSX focussed on discovering standalone gold and copper projects with > 1 Moz development potential. Novo is an innovative gold explorer with a significant land package covering approximately 5,500 square kilometres in the Pilbara region of Western Australia, along with the 22 square kilometre Belltopper project in the Bendigo Tectonic Zone of Victoria, Australia. In addition to the above, Novo is part of two prospective farm in agreements in New South Wales.
Novo’s key project area in the Pilbara is the Egina Gold Camp, where Northern Star Resources Limited (ASX: NST) is farming-in to form a JV at the Becher Project and surrounding tenements through exploration expenditure of A$25 million within 4 years for a 50% interest. The Becher Project has similar geological characteristics as Northern Star’s 12.7 Moz Hemi Project#. Novo is also advancing gold exploration south of Becher in the Egina Gold Camp, part of the Croydon JV (Novo 70%: Creasy Group 30%). Novo continues to undertake early-stage exploration elsewhere across its Pilbara tenement portfolio.
Novo has also formed a lithium joint venture with SQM in the Pilbara which provides shareholder exposure to battery metals.
Novo has recently strengthened its high-quality, Australian based exploration portfolio by adding the TechGen John Bull Gold Project in the New England Orogen of NSW, and Manhattan Tibooburra Gold Project in the Albert Goldfields in northwestern NSW. Both projects demonstrate prospectivity for significant discovery and resource definition and align with Novo’s strategy of identifying and exploring projects with > 1 Moz Au potential. These high-grade gold projects compliment the landholding consolidation that forms the Toolunga Project in the Onslow District in Western Australia.
Novo has a significant investment portfolio and a disciplined program in place to identify value accretive opportunities that will build further value for shareholders.
Please refer to Novo’s website for further information including the latest corporate presentation.

#Refer to De Grey’s ASX Announcement, Hemi Gold Project mineral Resource Estimate (MRE) 2024, dated 14 November 2024. No assurance can be given that a similar (or any) commercially viable mineral deposit will be determined at Novo’s Becher Project.
Appendix 1: Collar locations for Balla Balla AC program with peak downhole Au (ppb) listed. All coordinates are in GDA2020, zone 50.
Hole ID | Type | Depth | Easting (m) | Northing (m) | Dip | Azimuth (grid) | Peak Au (ppb) |
YUA0001 | AC | 21 | 601,556 | 7,717,479 | -60 | 140 | 3 |
YUA0002 | AC | 22 | 601,525 | 7,717,523 | -60 | 140 | 4 |
YUA0003 | AC | 21 | 601,488 | 7,717,559 | -60 | 140 | 2 |
YUA0004 | AC | 13 | 601,457 | 7,717,601 | -60 | 140 | 2 |
YUA0005 | AC | 14 | 601,423 | 7,717,640 | -60 | 140 | 1 |
YUA0006 | AC | 16 | 601,392 | 7,717,673 | -60 | 140 | 1 |
YUA0007 | AC | 13 | 601,853 | 7,718,124 | -60 | 140 | 1 |
YUA0008 | AC | 15 | 601,821 | 7,718,161 | -60 | 140 | 1 |
YUA0009 | AC | 13 | 601,787 | 7,718,203 | -60 | 140 | 4 |
YUA0010 | AC | 7 | 601,754 | 7,718,243 | -60 | 140 | -1 |
YUA0011 | AC | 5 | 601,725 | 7,718,279 | -60 | 140 | 1 |
YUA0012 | AC | 42 | 602,246 | 7,718,644 | -60 | 140 | 19 |
YUA0013 | AC | 36 | 602,217 | 7,718,684 | -60 | 140 | 3 |
YUA0014 | AC | 17 | 602,181 | 7,718,723 | -60 | 140 | 5 |
YUA0015 | AC | 16 | 602,153 | 7,718,762 | -60 | 140 | 10 |
YUA0016 | AC | 16 | 602,122 | 7,718,798 | -60 | 140 | 3 |
YUA0017 | AC | 21 | 602,549 | 7,719,288 | -60 | 140 | 4 |
YUA0018 | AC | 21 | 602,515 | 7,719,327 | -60 | 140 | 5 |
YUA0019 | AC | 60 | 602,484 | 7,719,368 | -60 | 140 | 11 |
YUA0020 | AC | 40 | 602,452 | 7,719,407 | -60 | 140 | 5 |
YUA0021 | AC | 23 | 602,418 | 7,719,446 | -60 | 140 | 17 |
YUA0022 | AC | 18 | 602,384 | 7,719,483 | -60 | 140 | 2 |
YUA0023 | AC | 27 | 603,830 | 7,719,250 | -60 | 140 | 14 |
YUA0024 | AC | 24 | 603,799 | 7,719,286 | -60 | 140 | 11 |
YUA0025 | AC | 30 | 603,768 | 7,719,326 | -60 | 140 | 17 |
YUA0026 | AC | 51 | 603,730 | 7,719,371 | -60 | 140 | 5 |
YUA0027 | AC | 30 | 603,700 | 7,719,408 | -60 | 140 | 20 |
YUA0028 | AC | 30 | 603,669 | 7,719,447 | -60 | 140 | 6 |
YUA0029 | AC | 33 | 603,635 | 7,719,484 | -60 | 140 | 15 |
YUA0030 | AC | 24 | 603,603 | 7,719,521 | -60 | 140 | 19 |
YUA0031 | AC | 21 | 603,576 | 7,719,558 | -60 | 140 | 3 |
YUA0032 | AC | 20 | 603,536 | 7,719,598 | -60 | 140 | 6 |
YUA0033 | AC | 22 | 603,505 | 7,719,635 | -60 | 140 | 8 |
YUA0034 | AC | 24 | 603,478 | 7,719,672 | -60 | 140 | 5 |
YUA0035 | AC | 22 | 603,446 | 7,719,713 | -60 | 140 | 13 |
YUA0036 | AC | 23 | 603,412 | 7,719,751 | -60 | 140 | 4 |
YUA0037 | AC | 27 | 603,381 | 7,719,793 | -60 | 140 | 4 |
YUA0038 | AC | 30 | 603,347 | 7,719,832 | -60 | 140 | 6 |
YUA0039 | AC | 39 | 603,316 | 7,719,869 | -60 | 140 | 8 |
YUA0040 | AC | 27 | 603,246 | 7,719,944 | -60 | 140 | 3 |
YUA0041 | AC | 39 | 603,218 | 7,719,980 | -60 | 140 | 13 |
YUA0042 | AC | 54 | 603,184 | 7,720,019 | -60 | 140 | 8 |
YUA0043 | AC | 27 | 603,156 | 7,720,065 | -60 | 140 | 9 |
YUA0044 | AC | 25 | 603,125 | 7,720,099 | -60 | 140 | 12 |
YUA0045 | AC | 20 | 603,091 | 7,720,134 | -60 | 140 | 9 |
YUA0046 | AC | 33 | 603,056 | 7,720,176 | -60 | 140 | 5 |
YUA0047 | AC | 42 | 603,025 | 7,720,212 | -60 | 140 | 9 |
YUA0048 | AC | 54 | 602,989 | 7,720,246 | -60 | 140 | 6 |
YUA0049 | AC | 27 | 602,958 | 7,720,281 | -60 | 140 | 4 |
YUA0050 | AC | 24 | 602,926 | 7,720,329 | -60 | 140 | 9 |
YUA0051 | AC | 34 | 602,896 | 7,720,369 | -60 | 140 | 7 |
YUA0052 | AC | 24 | 602,863 | 7,720,401 | -60 | 140 | 7 |
YUA0053 | AC | 26 | 605,416 | 7,719,348 | -60 | 140 | 8 |
YUA0054 | AC | 45 | 605,387 | 7,719,386 | -60 | 140 | 4 |
YUA0055 | AC | 45 | 605,353 | 7,719,429 | -60 | 140 | 5 |
YUA0056 | AC | 49 | 605,327 | 7,719,465 | -60 | 140 | 74 |
YUA0057 | AC | 30 | 605,291 | 7,719,505 | -60 | 140 | 11 |
YUA0058 | AC | 38 | 605,258 | 7,719,535 | -60 | 140 | 69 |
YUA0059 | AC | 30 | 605,223 | 7,719,581 | -60 | 140 | 6 |
YUA0060 | AC | 50 | 605,197 | 7,719,611 | -60 | 140 | 7 |
YUA0061 | AC | 15 | 605,159 | 7,719,657 | -60 | 140 | 2 |
YUA0062 | AC | 22 | 605,127 | 7,719,694 | -60 | 140 | 13 |
YUA0063 | AC | 13 | 605,100 | 7,719,736 | -60 | 140 | 2 |
YUA0064 | AC | 25 | 605,065 | 7,719,773 | -60 | 140 | 2 |
YUA0065 | AC | 25 | 605,031 | 7,719,810 | -60 | 140 | 2 |
YUA0066 | AC | 20 | 605,001 | 7,719,848 | -60 | 140 | 3 |
YUA0067 | AC | 23 | 605,423 | 7,721,826 | -60 | 140 | 2 |
YUA0068 | AC | 21 | 605,391 | 7,721,860 | -60 | 140 | 2 |
YUA0069 | AC | 21 | 605,361 | 7,721,901 | -60 | 140 | 2 |
YUA0070 | AC | 39 | 605,330 | 7,721,940 | -60 | 140 | 2 |
YUA0071 | AC | 31 | 605,298 | 7,721,986 | -60 | 140 | 5 |
YUA0072 | AC | 24 | 605,264 | 7,722,027 | -60 | 140 | 1 |
YUA0073 | AC | 19 | 605,235 | 7,722,061 | -60 | 140 | 1 |
YUA0074 | AC | 26 | 605,201 | 7,722,098 | -60 | 140 | 2 |
YUA0075 | AC | 20 | 605,163 | 7,722,136 | -60 | 140 | 1 |
YUA0076 | AC | 20 | 605,138 | 7,722,168 | -60 | 140 | 2 |
YUA0077 | AC | 20 | 605,101 | 7,722,213 | -60 | 140 | 3 |
YUA0078 | AC | 19 | 605,074 | 7,722,244 | -60 | 140 | 2 |
YUA0079 | AC | 24 | 605,981 | 7,722,165 | -60 | 140 | 3 |
YUA0080 | AC | 23 | 605,948 | 7,722,209 | -60 | 140 | 2 |
YUA0081 | AC | 24 | 605,916 | 7,722,247 | -60 | 140 | 4 |
YUA0082 | AC | 24 | 605,885 | 7,722,288 | -60 | 140 | 5 |
YUA0083 | AC | 25 | 605,851 | 7,722,329 | -60 | 140 | 3 |
YUA0084 | AC | 26 | 605,818 | 7,722,366 | -60 | 140 | 3 |
YUA0085 | AC | 28 | 605,784 | 7,722,401 | -60 | 140 | 3 |
YUA0086 | AC | 25 | 605,750 | 7,722,438 | -60 | 140 | 4 |
YUA0087 | AC | 28 | 605,718 | 7,722,478 | -60 | 140 | 4 |
YUA0088 | AC | 25 | 605,686 | 7,722,513 | -60 | 140 | 4 |
YUA0089 | AC | 26 | 605,654 | 7,722,560 | -60 | 140 | 3 |
YUA0090 | AC | 28 | 605,621 | 7,722,589 | -60 | 140 | 4 |
YUA0091 | AC | 25 | 605,595 | 7,722,632 | -60 | 140 | 10 |
YUA0092 | AC | 27 | 605,564 | 7,722,673 | -60 | 140 | 14 |
YUA0093 | AC | 26 | 605,530 | 7,722,711 | -60 | 140 | 6 |
YUA0094 | AC | 25 | 605,496 | 7,722,747 | -60 | 140 | 4 |
YUA0095 | AC | 26 | 605,463 | 7,722,783 | -60 | 140 | 3 |
YUA0096 | AC | 23 | 605,432 | 7,722,827 | -60 | 140 | 3 |
YUA0097 | AC | 23 | 605,403 | 7,722,864 | -60 | 140 | 4 |
YUA0098 | AC | 30 | 605,366 | 7,722,900 | -60 | 140 | 2 |
YUA0099 | AC | 25 | 605,332 | 7,722,938 | -60 | 140 | 5 |
YUA0100 | AC | 24 | 605,301 | 7,722,973 | -60 | 140 | 2 |
YUA0101 | AC | 25 | 605,267 | 7,723,012 | -60 | 140 | 6 |
YUA0102 | AC | 26 | 605,236 | 7,723,051 | -60 | 140 | 3 |
YUA0103 | AC | 26 | 607,502 | 7,723,836 | -60 | 140 | 1 |
YUA0104 | AC | 28 | 607,471 | 7,723,879 | -60 | 140 | 3 |
YUA0105 | AC | 29 | 607,435 | 7,723,917 | -60 | 140 | 20 |
YUA0106 | AC | 31 | 607,406 | 7,723,954 | -60 | 140 | 9 |
YUA0107 | AC | 30 | 607,374 | 7,723,986 | -60 | 140 | 5 |
YUA0108 | AC | 29 | 607,339 | 7,724,028 | -60 | 140 | 6 |
YUA0109 | AC | 33 | 607,305 | 7,724,067 | -60 | 140 | 4 |
YUA0110 | AC | 33 | 607,273 | 7,724,106 | -60 | 140 | 7 |
YUA0111 | AC | 32 | 607,241 | 7,724,144 | -60 | 140 | 3 |
YUA0112 | AC | 32 | 607,209 | 7,724,182 | -60 | 140 | 2 |
YUA0113 | AC | 29 | 607,177 | 7,724,221 | -60 | 140 | 2 |
YUA0114 | AC | 33 | 607,147 | 7,724,255 | -60 | 140 | 3 |
YUA0115 | AC | 29 | 607,116 | 7,724,292 | -60 | 140 | 2 |
YUA0116 | AC | 27 | 607,082 | 7,724,333 | -60 | 140 | 2 |
YUA0117 | AC | 25 | 607,051 | 7,724,374 | -60 | 140 | 1 |
YUA0118 | AC | 24 | 607,018 | 7,724,408 | -60 | 140 | 2 |
YUA0119 | AC | 22 | 606,987 | 7,724,438 | -60 | 140 | 3 |
YUA0120 | AC | 29 | 606,952 | 7,724,485 | -60 | 140 | 2 |
YUA0121 | AC | 25 | 606,922 | 7,724,518 | -60 | 140 | 2 |
YUA0122 | AC | 20 | 606,890 | 7,724,562 | -60 | 140 | 1 |
YUA0123 | AC | 20 | 606,857 | 7,724,602 | -60 | 140 | 2 |
YUA0124 | AC | 13 | 606,822 | 7,724,638 | -60 | 140 | 2 |
YUA0125 | AC | 13 | 606,794 | 7,724,679 | -60 | 140 | 1 |
YUA0126 | AC | 16 | 606,763 | 7,724,713 | -60 | 140 | 3 |
YUA0127 | AC | 20 | 606,736 | 7,724,759 | -60 | 140 | 3 |
YUA0128 | AC | 51 | 606,702 | 7,724,799 | -60 | 140 | 2 |
YUA0129 | AC | 52 | 606,667 | 7,724,840 | -60 | 140 | 3 |
YUA0130 | AC | 52 | 607,926 | 7,724,322 | -60 | 140 | 8 |
YUA0131 | AC | 27 | 607,892 | 7,724,361 | -60 | 140 | 4 |
YUA0132 | AC | 26 | 607,861 | 7,724,400 | -60 | 140 | 4 |
YUA0133 | AC | 24 | 607,830 | 7,724,438 | -60 | 140 | 3 |
YUA0134 | AC | 30 | 607,801 | 7,724,475 | -60 | 140 | 2 |
YUA0135 | AC | 22 | 607,767 | 7,724,513 | -60 | 140 | 4 |
YUA0136 | AC | 23 | 607,731 | 7,724,555 | -60 | 140 | 3 |
YUA0137 | AC | 26 | 607,699 | 7,724,594 | -60 | 140 | 3 |
YUA0138 | AC | 27 | 607,671 | 7,724,635 | -60 | 140 | 2 |
YUA0139 | AC | 20 | 607,635 | 7,724,674 | -60 | 140 | 3 |
YUA0140 | AC | 19 | 607,605 | 7,724,710 | -60 | 140 | 3 |
YUA0141 | AC | 23 | 610,801 | 7,720,407 | -60 | 140 | 3 |
YUA0142 | AC | 24 | 610,770 | 7,720,443 | -60 | 140 | 5 |
YUA0143 | AC | 39 | 610,735 | 7,720,480 | -60 | 140 | 6 |
YUA0144 | AC | 51 | 610,704 | 7,720,518 | -60 | 140 | 14 |
YUA0145 | AC | 72 | 610,668 | 7,720,556 | -60 | 140 | 7 |
YUA0146 | AC | 45 | 610,640 | 7,720,591 | -60 | 140 | 8 |
YUA0147 | AC | 36 | 610,611 | 7,720,634 | -60 | 140 | 3 |
YUA0148 | AC | 33 | 610,574 | 7,720,677 | -60 | 140 | 9 |
YUA0149 | AC | 60 | 610,541 | 7,720,713 | -60 | 140 | 21 |
YUA0150 | AC | 79 | 610,510 | 7,720,753 | -60 | 140 | 23 |
YUA0151 | AC | 62 | 610,478 | 7,720,787 | -60 | 140 | 34 |
YUA0152 | AC | 65 | 610,444 | 7,720,822 | -60 | 140 | 10 |
YUA0153 | AC | 55 | 610,411 | 7,720,866 | -60 | 140 | 9 |
YUA0154 | AC | 72 | 610,379 | 7,720,901 | -60 | 140 | 18 |
YUA0155 | AC | 72 | 610,348 | 7,720,938 | -60 | 140 | 31 |
YUA0156 | AC | 75 | 610,315 | 7,720,976 | -60 | 140 | 83 |
YUA0157 | AC | 69 | 610,283 | 7,721,014 | -60 | 140 | 9 |
YUA0158 | AC | 54 | 610,252 | 7,721,053 | -60 | 140 | 7 |
YUA0159 | AC | 60 | 610,219 | 7,721,091 | -60 | 140 | 29 |
YUA0160 | AC | 75 | 610,190 | 7,721,133 | -60 | 140 | 25 |
YUA0161 | AC | 78 | 610,157 | 7,721,174 | -60 | 140 | 16 |
YUA0162 | AC | 75 | 610,125 | 7,721,213 | -60 | 140 | 70 |
YUA0163 | AC | 60 | 610,088 | 7,721,250 | -60 | 140 | 16 |
YUA0164 | AC | 60 | 610,058 | 7,721,287 | -60 | 140 | 6 |
YUA0165 | AC | 57 | 610,024 | 7,721,327 | -60 | 140 | 3 |
YUA0166 | AC | 48 | 609,993 | 7,721,364 | -60 | 140 | 4 |
YUA0167 | AC | 69 | 609,965 | 7,721,402 | -60 | 140 | 15 |
YUA0168 | AC | 63 | 609,934 | 7,721,442 | -60 | 140 | 32 |
YUA0169 | AC | 18 | 611,128 | 7,721,015 | -60 | 140 | 2 |
YUA0170 | AC | 18 | 611,094 | 7,721,046 | -60 | 140 | 5 |
YUA0171 | AC | 21 | 611,066 | 7,721,092 | -60 | 140 | 5 |
YUA0172 | AC | 22 | 611,032 | 7,721,128 | -60 | 140 | 9 |
YUA0173 | AC | 20 | 611,001 | 7,721,163 | -60 | 140 | 2 |
YUA0174 | AC | 42 | 610,969 | 7,721,199 | -60 | 140 | 6 |
YUA0175 | AC | 28 | 610,938 | 7,721,239 | -60 | 140 | 47 |
YUA0176 | AC | 24 | 610,907 | 7,721,276 | -60 | 140 | 7 |
YUA0177 | AC | 29 | 610,876 | 7,721,317 | -60 | 140 | 5 |
YUA0178 | AC | 26 | 610,846 | 7,721,354 | -60 | 140 | 65 |
YUA0179 | AC | 35 | 610,808 | 7,721,394 | -60 | 140 | 41 |
YUA0180 | AC | 36 | 610,775 | 7,721,431 | -60 | 140 | 61 |
YUA0181 | AC | 48 | 610,748 | 7,721,459 | -60 | 140 | 4 |
YUA0182 | AC | 44 | 610,716 | 7,721,503 | -60 | 140 | 25 |
YUA0183 | AC | 50 | 610,680 | 7,721,539 | -60 | 140 | 114 |
YUA0184 | AC | 26 | 610,652 | 7,721,589 | -60 | 140 | 6 |
YUA0185 | AC | 45 | 610,617 | 7,721,631 | -60 | 140 | 28 |
YUA0186 | AC | 33 | 610,586 | 7,721,669 | -60 | 140 | 8 |
YUA0187 | AC | 78 | 610,555 | 7,721,704 | -60 | 140 | 7 |
Appendix 2: AC multi-element data for elements relevant to the mineralisation style and reported in this release. Bold values are considered anomalous for the district. Negative values are below detection.
Hole ID | From | To | Type | Au (ppb) | Ag (ppm) | Bi (ppm) | Cu (ppm) | Mo (ppm) | Sb (ppm) | Zn (ppm) | Te (ppm) |
YUA0001 | 20 | 21 | EOH | 2 | 0.05 | 0.25 | 24 | 0.6 | 3.5 | 95 | -0.05 |
YUA0002 | 21 | 22 | EOH | 4 | 0.03 | 0.16 | 26 | 0.6 | 1.4 | 72 | -0.05 |
YUA0003 | 20 | 21 | EOH | 2 | 0.07 | 0.04 | 55 | 3.1 | 0.7 | 134 | -0.05 |
YUA0004 | 12 | 13 | EOH | 1 | 0.15 | 0.03 | 18 | 0.5 | 0.3 | 72 | -0.05 |
YUA0005 | 13 | 14 | EOH | 1 | 0.25 | 0.03 | 21 | 0.7 | 0.2 | 113 | -0.05 |
YUA0006 | 15 | 16 | EOH | 1 | 0.08 | 0.05 | 22 | 0.6 | 0.2 | 125 | -0.05 |
YUA0007 | 12 | 13 | EOH | 1 | 0.05 | 0.05 | 10 | 0.5 | 2.2 | 85 | 0.05 |
YUA0008 | 13 | 14 | EOH | 1 | 0.05 | 0.04 | 6 | 0.3 | 1.1 | 124 | -0.05 |
YUA0009 | 12 | 13 | EOH | 4 | 0.03 | 0.03 | 18 | 0.4 | 1.4 | 131 | -0.05 |
YUA0010 | 6 | 7 | EOH | -1 | 0.03 | 0.03 | 21 | 0.4 | 1.0 | 147 | -0.05 |
YUA0011 | 4 | 5 | EOH | 1 | 0.15 | 0.04 | 19 | 0.6 | 1.1 | 111 | -0.05 |
YUA0012 | 41 | 42 | EOH | 3 | 0.06 | 0.11 | 13 | 2.5 | 2.9 | 31 | -0.05 |
YUA0013 | 35 | 36 | EOH | -1 | 0.07 | 0.01 | 70 | 0.5 | 7.2 | 218 | -0.05 |
YUA0014 | 16 | 17 | EOH | 3 | 4.74 | 0.04 | 13 | 1.6 | 0.8 | 30 | -0.05 |
YUA0015 | 15 | 16 | EOH | 10 | 0.32 | 0.04 | 10 | 0.6 | 0.4 | 16 | -0.05 |
YUA0016 | 15 | 16 | EOH | 3 | 0.17 | 0.06 | 11 | 0.4 | 0.6 | 22 | -0.05 |
YUA0017 | 20 | 21 | EOH | 3 | 0.09 | 0.01 | 48 | 0.3 | 16.6 | 309 | -0.05 |
YUA0018 | 20 | 21 | EOH | 3 | 0.16 | 0.04 | 107 | 0.3 | 5.0 | 409 | 0.05 |
YUA0019 | 59 | 60 | EOH | 4 | 0.05 | 0.13 | 65 | 0.3 | 3.3 | 109 | -0.05 |
YUA0020 | 39 | 40 | EOH | 4 | 0.07 | 0.04 | 17 | 0.7 | 3.1 | 110 | -0.05 |
YUA0021 | 22 | 23 | EOH | 2 | 0.10 | 0.06 | 32 | 6.5 | 2.2 | 89 | -0.05 |
YUA0022 | 17 | 18 | EOH | 1 | 0.09 | 0.10 | 20 | 0.6 | 1.2 | 27 | -0.05 |
YUA0023 | 26 | 27 | EOH | 6 | 0.74 | 0.14 | 23 | 0.8 | 2.2 | 54 | -0.05 |
YUA0024 | 23 | 24 | EOH | 4 | 0.09 | 0.14 | 58 | 1.0 | 4.5 | 41 | -0.05 |
YUA0025 | 29 | 30 | EOH | 1 | 0.04 | 0.17 | 21 | 0.6 | 8.4 | 10 | -0.05 |
YUA0026 | 50 | 51 | EOH | -1 | 0.09 | -0.01 | 165 | 0.5 | 3.9 | 117 | -0.05 |
YUA0027 | 29 | 30 | EOH | 1 | 0.04 | 0.01 | 50 | 0.2 | 11.9 | 124 | -0.05 |
YUA0028 | 29 | 30 | EOH | 1 | 0.09 | 0.05 | 215 | 0.9 | 10.4 | 130 | 0.07 |
YUA0029 | 32 | 33 | EOH | 3 | 0.06 | 0.06 | 93 | 0.3 | 4.3 | 104 | -0.05 |
YUA0030 | 23 | 24 | EOH | 19 | 0.04 | 0.03 | 82 | 0.2 | 3.6 | 72 | -0.05 |
YUA0031 | 20 | 21 | EOH | 3 | 0.03 | 0.03 | 54 | 0.2 | 2.3 | 77 | -0.05 |
YUA0032 | 19 | 20 | EOH | 1 | 0.04 | 0.07 | 21 | 0.3 | 1.3 | 42 | -0.05 |
YUA0033 | 21 | 22 | EOH | 2 | 0.05 | 0.14 | 52 | 0.4 | 1.7 | 56 | -0.05 |
YUA0034 | 23 | 24 | EOH | -1 | 0.09 | 0.06 | 18 | 0.5 | 1.5 | 36 | -0.05 |
YUA0035 | 21 | 22 | EOH | -1 | 0.09 | 0.11 | 35 | 0.7 | 1.9 | 327 | -0.05 |
YUA0036 | 22 | 23 | EOH | -1 | 0.03 | 0.09 | 23 | 0.5 | 1.7 | 66 | -0.05 |
YUA0037 | 26 | 27 | EOH | -1 | 0.52 | 0.16 | 32 | 0.3 | 2.6 | 381 | -0.05 |
YUA0038 | 29 | 30 | EOH | 2 | 0.47 | 0.03 | 83 | 0.4 | 4.0 | 85 | -0.05 |
YUA0039 | 38 | 39 | EOH | 8 | 0.03 | 0.03 | 64 | 0.2 | 2.9 | 88 | -0.05 |
YUA0040 | 26 | 27 | EOH | 1 | 0.08 | 0.01 | 74 | 0.5 | 2.3 | 16 | -0.05 |
YUA0041 | 38 | 39 | EOH | 5 | 0.20 | -0.01 | 98 | 0.7 | 6.7 | 169 | -0.05 |
YUA0042 | 53 | 54 | EOH | 4 | 0.20 | -0.01 | 120 | 0.6 | 5.3 | 96 | -0.05 |
YUA0043 | 26 | 27 | EOH | 9 | 0.21 | -0.01 | 75 | 7.4 | 5.2 | 219 | -0.05 |
YUA0044 | 24 | 25 | EOH | 3 | 0.06 | -0.01 | 77 | 1.0 | 1.5 | 228 | -0.05 |
YUA0045 | 19 | 20 | EOH | 9 | 0.05 | -0.01 | 61 | 0.4 | 1.8 | 54 | -0.05 |
YUA0046 | 32 | 33 | EOH | 1 | 0.03 | -0.01 | 103 | 0.4 | 2.4 | 115 | -0.05 |
YUA0047 | 41 | 42 | EOH | 4 | 0.05 | -0.01 | 40 | 0.2 | 1.8 | 90 | -0.05 |
YUA0048 | 53 | 54 | EOH | 1 | 0.02 | -0.01 | 64 | 0.2 | 2.2 | 58 | -0.05 |
YUA0049 | 26 | 27 | EOH | 1 | 0.14 | -0.01 | 114 | 0.3 | 1.4 | 108 | -0.05 |
YUA0050 | 23 | 24 | EOH | 3 | 0.10 | -0.01 | 52 | 1.4 | 2.7 | 183 | -0.05 |
YUA0051 | 33 | 34 | EOH | 3 | 0.06 | 0.07 | 23 | 0.9 | 1.4 | 43 | -0.05 |
YUA0052 | 23 | 24 | EOH | 4 | 0.11 | 0.08 | 18 | 0.4 | 1.3 | 45 | -0.05 |
YUA0053 | 25 | 26 | EOH | 1 | 0.17 | -0.01 | 178 | 1.0 | 13.4 | 73 | -0.05 |
YUA0054 | 15 | 18 | Comp | 2 | 0.09 | 0.03 | 63 | 0.7 | 5.2 | 62 | 0.025 |
YUA0054 | 18 | 21 | Comp | 2 | 0.18 | 0.03 | 108 | 1.1 | 7.9 | 96 | 0.025 |
YUA0054 | 21 | 24 | Comp | 2 | 0.15 | 0.03 | 102 | 1.2 | 5.8 | 84 | 0.025 |
YUA0054 | 24 | 27 | Comp | 1 | 0.09 | 0.03 | 90 | 1.3 | 7.6 | 74 | 0.025 |
YUA0054 | 27 | 30 | Comp | 1 | 0.07 | 0.04 | 100 | 1.3 | 8.1 | 86 | 0.025 |
YUA0054 | 30 | 33 | Comp | 3 | 0.05 | 0.03 | 97 | 1.1 | 4.7 | 95 | 0.025 |
YUA0054 | 33 | 36 | Comp | 2 | 0.07 | 0.02 | 111 | 1.6 | 51.6 | 89 | 0.025 |
YUA0054 | 36 | 39 | Comp | 1 | 0.13 | 0.09 | 48 | 1.1 | 145.5 | 53 | 0.025 |
YUA0054 | 39 | 42 | Comp | 2 | 0.11 | 0.15 | 39 | 0.8 | 19.3 | 40 | 0.025 |
YUA0054 | 42 | 44 | Comp | 4 | 0.05 | 0.04 | 92 | 1.5 | 82.3 | 56 | 0.025 |
YUA0054 | 44 | 45 | EOH | 3 | 6.72 | -0.01 | 48 | 3.4 | 182.0 | 75 | -0.05 |
YUA0055 | 0 | 3 | Comp | 2 | 0.02 | 0.09 | 15 | 0.4 | 0.5 | 12 | 0.025 |
YUA0055 | 44 | 45 | EOH | 3 | 0.11 | 0.19 | 72 | 1.2 | 8.2 | 123 | -0.05 |
YUA0056 | 21 | 24 | Comp | 22 | 0.29 | 0.11 | 13 | 1.1 | 7.5 | 14 | 0.025 |
YUA0056 | 24 | 27 | Comp | 39 | 0.17 | 0.11 | 22 | 1.2 | 11.2 | 9 | 0.025 |
YUA0056 | 27 | 30 | Comp | 74 | 0.08 | 0.21 | 54 | 1.5 | 16.6 | 12 | 0.025 |
YUA0056 | 30 | 33 | Comp | 48 | 0.11 | 0.17 | 31 | 1.2 | 15.8 | 30 | 0.025 |
YUA0056 | 33 | 36 | Comp | 42 | 0.16 | 0.19 | 29 | 1.1 | 13.1 | 38 | 0.025 |
YUA0056 | 36 | 39 | Comp | 14 | 0.05 | 0.16 | 21 | 0.5 | 3.9 | 26 | 0.025 |
YUA0056 | 39 | 42 | Comp | 13 | 0.06 | 0.14 | 26 | 0.7 | 5.5 | 35 | 0.025 |
YUA0056 | 42 | 45 | Comp | 66 | 0.12 | 0.15 | 27 | 0.9 | 7.1 | 30 | 0.025 |
YUA0056 | 45 | 48 | Comp | 44 | 0.20 | 0.17 | 38 | 1.3 | 15.6 | 36 | 0.025 |
YUA0056 | 48 | 49 | EOH | 13 | 0.13 | 0.02 | 17 | 1.0 | 4.9 | 18 | -0.05 |
YUA0057 | 29 | 30 | EOH | 2 | 0.37 | 0.04 | 24 | 1.5 | 1.9 | 13 | -0.05 |
YUA0058 | 37 | 38 | EOH | 3 | 3.28 | -0.01 | 13 | 5.6 | 1.4 | 5 | -0.05 |
YUA0059 | 29 | 30 | EOH | 5 | 0.05 | -0.01 | 186 | 1.2 | 2.9 | 126 | -0.05 |
YUA0060 | 49 | 50 | EOH | 2 | 0.08 | -0.01 | 148 | 0.8 | 1.3 | 107 | -0.05 |
YUA0061 | 14 | 15 | EOH | 1 | 0.04 | 0.02 | 10 | 0.5 | 0.6 | 31 | -0.05 |
YUA0062 | 21 | 22 | EOH | 6 | 2.75 | 0.09 | 65 | 0.7 | 1.1 | 64 | -0.05 |
YUA0063 | 12 | 13 | EOH | 1 | 0.11 | -0.01 | 16 | 0.7 | 0.4 | 20 | -0.05 |
YUA0064 | 24 | 25 | EOH | 1 | 0.24 | 0.52 | 23 | 0.7 | 1.2 | 35 | -0.05 |
YUA0065 | 24 | 25 | EOH | 2 | 0.17 | 0.02 | 18 | 0.7 | 0.9 | 67 | -0.05 |
YUA0066 | 19 | 20 | EOH | 3 | 0.19 | 0.04 | 19 | 0.6 | 1.0 | 56 | -0.05 |
YUA0067 | 22 | 23 | EOH | 1 | 0.41 | 0.21 | 7 | 0.7 | 5.2 | 62 | -0.05 |
YUA0068 | 20 | 21 | EOH | 2 | 0.07 | 0.08 | 11 | 1.5 | 5.7 | 53 | -0.05 |
YUA0069 | 20 | 21 | EOH | 1 | 0.25 | 0.01 | 7 | 1.0 | 4.6 | 61 | -0.05 |
YUA0070 | 38 | 39 | EOH | -1 | 0.08 | 0.21 | 7 | 0.7 | 6.2 | 81 | -0.05 |
YUA0071 | 30 | 31 | EOH | -1 | 0.06 | 0.11 | 4 | 0.7 | 5.7 | 75 | -0.05 |
YUA0072 | 23 | 24 | EOH | -1 | 0.08 | 0.11 | 10 | 0.9 | 3.1 | 50 | -0.05 |
YUA0073 | 18 | 19 | EOH | 1 | 0.13 | 0.06 | 8 | 1.8 | 3.6 | 46 | -0.05 |
YUA0074 | 25 | 26 | EOH | 1 | 0.06 | 0.11 | 4 | 1.3 | 6.9 | 79 | -0.05 |
YUA0075 | 19 | 20 | EOH | 1 | 0.02 | 0.03 | 11 | 0.7 | 2.2 | 28 | -0.05 |
YUA0076 | 19 | 20 | EOH | 1 | 0.27 | 0.07 | 8 | 1.8 | 2.6 | 39 | -0.05 |
YUA0077 | 18 | 19 | EOH | 1 | 0.17 | 0.09 | 23 | 1.2 | 2.4 | 26 | -0.05 |
YUA0078 | 18 | 19 | EOH | 1 | 0.11 | 0.17 | 5 | 1.9 | 3.8 | 89 | -0.05 |
YUA0079 | 23 | 24 | EOH | 2 | 0.12 | 0.30 | 18 | 6.8 | 12.6 | 77 | 0.07 |
YUA0080 | 22 | 23 | EOH | 2 | 7.14 | 0.12 | 21 | 1.7 | 4.6 | 26 | -0.05 |
YUA0081 | 23 | 24 | EOH | 2 | 0.32 | 0.10 | 12 | 1.1 | 9.6 | 20 | -0.05 |
YUA0082 | 23 | 24 | EOH | 2 | 0.03 | 0.11 | 13 | 0.4 | 4.5 | 27 | -0.05 |
YUA0083 | 24 | 25 | EOH | 3 | 0.04 | 0.09 | 8 | 0.5 | 2.5 | 23 | -0.05 |
YUA0084 | 25 | 26 | EOH | 2 | 0.05 | 0.12 | 21 | 0.5 | 5.3 | 39 | -0.05 |
YUA0085 | 27 | 28 | EOH | 2 | 0.08 | 0.13 | 16 | 0.7 | 6.8 | 41 | -0.05 |
YUA0086 | 24 | 25 | EOH | 4 | 0.09 | 0.20 | 21 | 0.8 | 7.0 | 44 | -0.05 |
YUA0087 | 27 | 28 | EOH | 3 | 0.47 | 0.41 | 22 | 1.1 | 5.8 | 100 | -0.05 |
YUA0088 | 24 | 25 | EOH | 4 | 0.13 | 0.06 | 10 | 0.3 | 2.2 | 18 | -0.05 |
YUA0089 | 25 | 26 | EOH | 2 | 0.24 | 0.43 | 18 | 0.9 | 7.5 | 79 | -0.05 |
YUA0090 | 27 | 28 | EOH | 2 | 0.11 | 0.14 | 20 | 0.5 | 3.3 | 52 | -0.05 |
YUA0091 | 24 | 25 | EOH | 2 | 0.09 | 0.12 | 16 | 0.7 | 3.9 | 32 | -0.05 |
YUA0092 | 26 | 27 | EOH | 3 | 0.08 | 0.15 | 24 | 0.5 | 2.7 | 35 | -0.05 |
YUA0093 | 25 | 26 | EOH | 2 | 0.16 | 0.45 | 12 | 0.6 | 4.4 | 52 | -0.05 |
YUA0094 | 24 | 25 | EOH | 2 | 0.19 | 0.18 | 12 | 1.1 | 5.3 | 80 | -0.05 |
YUA0095 | 25 | 26 | EOH | 2 | 7.05 | 0.25 | 37 | 1.8 | 8.5 | 78 | -0.05 |
YUA0096 | 22 | 23 | EOH | 2 | 0.42 | 0.13 | 13 | 1.6 | 4.6 | 43 | -0.05 |
YUA0097 | 22 | 23 | EOH | 2 | 0.05 | 0.11 | 13 | 1.2 | 7.6 | 51 | -0.05 |
YUA0098 | 29 | 30 | EOH | 2 | 0.04 | 0.07 | 14 | 0.5 | 1.9 | 26 | -0.05 |
YUA0099 | 24 | 25 | EOH | 2 | 0.12 | 0.20 | 10 | 0.7 | 8.2 | 59 | -0.05 |
YUA0100 | 23 | 24 | EOH | 2 | 0.05 | 0.08 | 6 | 0.7 | 6.3 | 77 | -0.05 |
YUA0101 | 24 | 25 | EOH | 1 | 0.23 | 0.08 | 7 | 0.7 | 3.1 | 53 | -0.05 |
YUA0102 | 25 | 26 | EOH | 1 | 0.14 | 0.17 | 8 | 1.3 | 7.1 | 76 | -0.05 |
YUA0103 | 25 | 26 | EOH | 1 | 0.07 | 0.13 | 20 | 0.7 | 4.0 | 26 | -0.05 |
YUA0104 | 27 | 28 | EOH | 2 | 0.08 | 0.09 | 10 | 0.5 | 2.8 | 28 | -0.05 |
YUA0105 | 28 | 29 | EOH | 4 | 0.18 | 0.09 | 18 | 1.0 | 6.9 | 31 | -0.05 |
YUA0106 | 30 | 31 | EOH | 2 | 0.11 | 0.16 | 22 | 0.6 | 21.3 | 78 | -0.05 |
YUA0107 | 29 | 30 | EOH | 2 | 0.12 | 0.09 | 11 | 0.5 | 17.1 | 60 | -0.05 |
YUA0108 | 28 | 29 | EOH | 3 | 0.04 | 0.09 | 11 | 0.4 | 4.7 | 31 | -0.05 |
YUA0109 | 32 | 33 | EOH | 3 | 0.03 | 0.06 | 16 | 0.6 | 3.7 | 56 | -0.05 |
YUA0110 | 32 | 33 | EOH | 2 | 0.05 | 0.14 | 16 | 0.5 | 7.8 | 47 | -0.05 |
YUA0111 | 31 | 32 | EOH | 2 | 0.07 | 0.16 | 14 | 0.5 | 5.9 | 32 | -0.05 |
YUA0112 | 30 | 31 | EOH | 2 | 0.06 | 0.14 | 19 | 0.6 | 5.6 | 31 | -0.05 |
YUA0113 | 28 | 29 | EOH | 2 | 96.80 | 0.83 | 78 | 2.1 | 8.1 | 112 | -0.05 |
YUA0114 | 32 | 33 | EOH | 2 | 0.18 | 0.14 | 18 | 0.6 | 3.0 | 50 | -0.05 |
YUA0115 | 28 | 29 | EOH | 2 | 0.62 | 12.50 | 9 | 0.9 | 5.6 | 51 | 0.15 |
YUA0116 | 26 | 27 | EOH | 2 | 0.74 | 0.32 | 18 | 1.3 | 4.6 | 47 | -0.05 |
YUA0117 | 24 | 25 | EOH | 1 | 0.08 | 0.20 | 13 | 0.8 | 6.5 | 65 | -0.05 |
YUA0118 | 23 | 24 | EOH | 2 | 0.16 | 0.21 | 17 | 0.5 | 3.9 | 47 | -0.05 |
YUA0119 | 21 | 22 | EOH | 3 | 0.14 | 0.21 | 25 | 0.9 | 6.1 | 44 | 0.05 |
YUA0120 | 28 | 29 | EOH | 2 | 0.07 | 0.05 | 8 | 0.4 | 5.5 | 75 | -0.05 |
YUA0121 | 24 | 25 | EOH | 2 | 0.03 | 0.08 | 5 | 0.4 | 5.3 | 79 | -0.05 |
YUA0122 | 19 | 20 | EOH | 1 | 0.42 | 0.11 | 8 | 0.6 | 3.7 | 64 | -0.05 |
YUA0123 | 17 | 18 | EOH | 2 | 0.38 | 0.07 | 10 | 0.7 | 1.5 | 31 | -0.05 |
YUA0124 | 12 | 13 | EOH | 2 | 9.76 | 0.12 | 11 | 2.6 | 4.4 | 70 | -0.05 |
YUA0125 | 12 | 13 | EOH | 1 | 0.32 | 0.15 | 6 | 5.3 | 3.2 | 80 | -0.05 |
YUA0126 | 15 | 16 | EOH | 3 | 0.77 | 0.13 | 20 | 1.4 | 1.3 | 43 | -0.05 |
YUA0127 | 19 | 20 | EOH | 3 | 21.70 | 0.11 | 24 | 3.8 | 1.9 | 51 | -0.05 |
YUA0128 | 50 | 51 | EOH | 2 | 0.11 | 0.07 | 16 | 0.7 | 1.9 | 63 | -0.05 |
YUA0129 | 51 | 52 | EOH | 3 | 0.13 | 0.12 | 18 | 0.5 | 2.8 | 65 | -0.05 |
YUA0130 | 26 | 27 | EOH | 8 | 0.15 | 0.13 | 13 | 0.9 | 3.4 | 29 | -0.05 |
YUA0131 | 26 | 27 | EOH | 4 | 0.13 | 0.11 | 17 | 0.5 | 2.6 | 27 | -0.05 |
YUA0132 | 25 | 26 | EOH | 4 | 0.27 | 0.10 | 13 | 0.9 | 2.2 | 22 | -0.05 |
YUA0133 | 23 | 24 | EOH | 3 | 0.13 | 0.10 | 13 | 1.1 | 14.0 | 69 | -0.05 |
YUA0134 | 29 | 30 | EOH | 2 | 0.06 | 0.18 | 4 | 0.8 | 14.4 | 94 | -0.05 |
YUA0135 | 21 | 22 | EOH | 4 | 0.37 | 0.09 | 7 | 0.9 | 7.5 | 72 | -0.05 |
YUA0136 | 22 | 23 | EOH | 3 | 0.51 | 0.12 | 10 | 1.0 | 6.2 | 66 | -0.05 |
YUA0137 | 25 | 26 | EOH | 3 | 0.66 | 0.14 | 8 | 0.8 | 4.8 | 48 | -0.05 |
YUA0138 | 26 | 27 | EOH | 2 | 3.54 | 0.22 | 9 | 2.4 | 9.0 | 91 | -0.05 |
YUA0139 | 19 | 20 | EOH | 3 | 0.97 | 0.13 | 12 | 1.3 | 5.6 | 58 | -0.05 |
YUA0140 | 18 | 19 | EOH | 3 | 0.17 | 0.10 | 11 | 1.0 | 5.6 | 57 | -0.05 |
YUA0141 | 22 | 23 | EOH | 3 | 0.17 | 0.35 | 11 | 4.6 | 3.5 | 23 | -0.05 |
YUA0142 | 23 | 24 | EOH | 5 | 0.15 | 0.33 | 5 | 1.4 | 4.1 | 16 | -0.05 |
YUA0143 | 38 | 39 | EOH | 6 | 0.04 | 0.13 | 7 | 2.3 | 3.7 | 66 | -0.05 |
YUA0144 | 50 | 51 | EOH | 14 | 0.09 | 0.14 | 28 | 4.5 | 10.5 | 90 | -0.05 |
YUA0145 | 71 | 72 | EOH | 7 | 0.05 | 0.22 | 56 | 2.3 | 3.4 | 85 | 0.14 |
YUA0146 | 44 | 45 | EOH | 8 | 0.21 | 0.30 | 37 | 1.1 | 3.6 | 80 | 0.07 |
YUA0147 | 35 | 36 | EOH | 3 | 0.07 | 0.59 | 211 | 2.1 | 3.7 | 158 | 0.13 |
YUA0148 | 32 | 33 | EOH | 1 | 0.15 | 0.29 | 77 | 1.2 | 2.6 | 114 | 0.21 |
YUA0149 | 59 | 60 | EOH | 5 | 0.06 | 0.31 | 48 | 1.6 | 6.2 | 99 | 0.25 |
YUA0150 | 78 | 79 | EOH | 9 | 0.09 | 0.23 | 65 | 1.6 | 6.0 | 136 | 0.24 |
YUA0151 | 61 | 62 | EOH | 4 | 0.11 | 0.31 | 70 | 1.7 | 7.8 | 141 | 0.1 |
YUA0152 | 64 | 65 | EOH | 3 | 0.09 | 0.46 | 71 | 1.7 | 3.5 | 107 | 0.25 |
YUA0153 | 54 | 55 | EOH | 6 | 0.05 | 0.57 | 88 | 1.5 | 5.0 | 126 | 0.21 |
YUA0154 | 71 | 72 | EOH | 8 | 0.05 | 0.62 | 46 | 1.7 | 2.8 | 100 | 0.11 |
YUA0155 | 71 | 72 | EOH | 3 | 0.06 | 0.42 | 63 | 0.7 | 3.6 | 106 | 0.07 |
YUA0156 | 74 | 75 | EOH | 7 | 0.09 | 0.76 | 84 | 1.8 | 2.5 | 96 | 0.24 |
YUA0157 | 68 | 69 | EOH | 5 | 0.29 | 1.08 | 98 | 1.5 | 7.3 | 278 | 0.25 |
YUA0158 | 53 | 54 | EOH | 7 | 0.06 | 0.37 | 65 | 0.9 | 5.2 | 175 | 0.12 |
YUA0159 | 59 | 60 | EOH | 6 | 0.06 | 0.86 | 56 | 0.7 | 4.6 | 144 | 0.12 |
YUA0160 | 21 | 24 | Comp | 4 | 0.05 | 0.22 | 23 | 0.7 | 1.0 | 31 | -0.05 |
YUA0160 | 24 | 27 | Comp | 4 | 0.06 | 0.20 | 23 | 0.8 | 1.2 | 28 | -0.05 |
YUA0160 | 27 | 30 | Comp | 2 | 0.23 | 0.41 | 32 | 0.3 | 2.3 | 40 | 0.14 |
YUA0160 | 30 | 33 | Comp | 1 | 0.13 | 0.71 | 55 | 0.5 | 6.6 | 87 | 0.38 |
YUA0160 | 33 | 36 | Comp | 2 | 0.09 | 1.20 | 47 | 0.5 | 5.3 | 104 | 0.3 |
YUA0160 | 36 | 39 | Comp | 2 | 0.05 | 1.61 | 30 | 0.7 | 6.0 | 93 | 0.33 |
YUA0160 | 39 | 42 | Comp | 5 | 0.05 | 2.82 | 48 | 0.7 | 6.5 | 153 | 0.37 |
YUA0160 | 42 | 45 | Comp | 7 | 0.07 | 1.50 | 49 | 0.6 | 4.9 | 141 | 0.32 |
YUA0160 | 45 | 48 | Comp | 18 | 0.14 | 1.69 | 61 | 1.5 | 9.1 | 119 | 0.6 |
YUA0160 | 48 | 51 | Comp | 25 | 0.20 | 7.19 | 99 | 3.0 | 11.1 | 82 | 2.25 |
YUA0160 | 51 | 54 | Comp | 6 | 0.09 | 3.34 | 75 | 2.0 | 12.6 | 102 | 1.11 |
YUA0160 | 54 | 57 | Comp | 3 | 0.06 | 0.79 | 44 | 0.8 | 6.8 | 103 | 0.26 |
YUA0160 | 57 | 60 | Comp | 5 | 0.06 | 0.88 | 36 | 0.9 | 5.5 | 95 | 0.35 |
YUA0160 | 60 | 63 | Comp | 4 | 0.14 | 5.18 | 60 | 1.5 | 6.1 | 107 | 1.01 |
YUA0160 | 63 | 66 | Comp | 5 | 0.14 | 3.91 | 71 | 2.6 | 5.3 | 119 | 1.07 |
YUA0160 | 66 | 69 | Comp | 4 | 0.08 | 2.63 | 83 | 1.7 | 5.4 | 121 | 0.42 |
YUA0160 | 69 | 72 | Comp | 4 | 0.06 | 2.39 | 77 | 3.5 | 5.1 | 140 | 0.34 |
YUA0160 | 72 | 74 | Comp | 3 | 0.05 | 0.46 | 94 | 1.0 | 4.8 | 134 | 0.11 |
YUA0160 | 74 | 75 | EOH | 5 | 0.07 | 1.16 | 76 | 1.1 | 7.3 | 141 | 0.31 |
YUA0161 | 21 | 24 | Comp | 3 | 0.09 | 0.20 | 20 | 0.6 | 0.8 | 28 | 0.05 |
YUA0161 | 24 | 27 | Comp | 3 | 0.13 | 0.35 | 24 | 0.8 | 1.6 | 32 | 0.06 |
YUA0161 | 27 | 30 | Comp | 3 | 0.20 | 0.65 | 27 | 0.4 | 4.9 | 37 | 0.17 |
YUA0161 | 30 | 33 | Comp | 1 | 0.21 | 1.26 | 66 | 1.1 | 3.9 | 67 | 0.5 |
YUA0161 | 33 | 36 | Comp | 2 | 0.40 | 0.46 | 73 | 1.2 | 4.3 | 133 | 0.2 |
YUA0161 | 36 | 39 | Comp | 2 | 0.33 | 0.44 | 68 | 1.2 | 4.7 | 165 | 0.18 |
YUA0161 | 39 | 42 | Comp | -1 | 0.17 | 0.90 | 50 | 1.7 | 5.1 | 141 | 0.5 |
YUA0161 | 42 | 45 | Comp | 4 | 0.05 | 1.26 | 71 | 1.7 | 6.6 | 131 | 0.49 |
YUA0161 | 45 | 48 | Comp | 10 | 0.07 | 1.29 | 89 | 0.8 | 7.7 | 173 | 0.48 |
YUA0161 | 48 | 51 | Comp | 2 | 0.02 | 0.58 | 51 | 1.2 | 4.8 | 150 | 0.17 |
YUA0161 | 51 | 54 | Comp | 8 | 0.08 | 1.34 | 54 | 2.5 | 5.0 | 127 | 0.27 |
YUA0161 | 54 | 57 | Comp | 6 | 0.07 | 1.72 | 15 | 5.6 | 6.1 | 123 | 0.44 |
YUA0161 | 57 | 60 | Comp | 6 | 0.17 | 15.80 | 63 | 5.3 | 14.3 | 194 | 0.97 |
YUA0161 | 60 | 63 | Comp | 4 | 0.15 | 7.23 | 114 | 6.5 | 47.3 | 447 | 1.25 |
YUA0161 | 63 | 66 | Comp | 14 | 1.31 | 2.52 | 36 | 5.6 | 12.0 | 132 | 0.64 |
YUA0161 | 66 | 69 | Comp | 10 | 0.20 | 5.05 | 48 | 2.0 | 17.2 | 132 | 0.81 |
YUA0161 | 69 | 72 | Comp | 9 | 0.51 | 3.55 | 57 | 1.9 | 12.5 | 107 | 0.62 |
YUA0161 | 72 | 75 | Comp | 16 | 0.09 | 2.31 | 71 | 1.8 | 11.0 | 81 | 1.02 |
YUA0161 | 75 | 77 | Comp | 8 | 0.23 | 16.45 | 53 | 1.3 | 4.4 | 122 | 1.14 |
YUA0161 | 77 | 78 | EOH | 5 | 0.11 | 71.60 | 111 | 1.7 | 6.4 | 116 | 6.23 |
YUA0162 | 18 | 21 | Comp | 12 | 0.25 | 0.10 | 17 | 0.6 | 0.5 | 22 | -0.05 |
YUA0162 | 21 | 24 | Comp | 13 | 0.08 | 0.32 | 20 | 0.7 | 0.6 | 27 | -0.05 |
YUA0162 | 24 | 27 | Comp | 9 | 0.08 | 0.16 | 19 | 0.8 | 1.2 | 30 | 0.05 |
YUA0162 | 27 | 30 | Comp | 9 | 0.16 | 0.53 | 18 | 0.4 | 2.2 | 21 | 0.11 |
YUA0162 | 30 | 33 | Comp | 4 | 0.18 | 1.15 | 13 | 0.6 | 6.2 | 16 | 0.45 |
YUA0162 | 33 | 36 | Comp | 2 | 0.05 | 1.98 | 17 | 1.9 | 7.3 | 17 | 1.05 |
YUA0162 | 36 | 39 | Comp | 1 | 0.08 | 2.13 | 13 | 1.4 | 11.0 | 14 | 1.29 |
YUA0162 | 39 | 42 | Comp | 3 | 0.08 | 7.51 | 20 | 7.4 | 8.1 | 32 | 3.59 |
YUA0162 | 42 | 45 | Comp | 4 | 0.09 | 2.25 | 13 | 12.2 | 5.9 | 28 | 0.84 |
YUA0162 | 45 | 48 | Comp | 13 | 0.12 | 11.45 | 18 | 44.3 | 5.3 | 47 | 2.57 |
YUA0162 | 48 | 51 | Comp | 9 | 0.11 | 8.36 | 22 | 58.4 | 5.9 | 60 | 2.14 |
YUA0162 | 51 | 54 | Comp | 54 | 0.28 | 14.50 | 21 | 31.4 | 6.4 | 63 | 11.8 |
YUA0162 | 54 | 57 | Comp | 21 | 0.23 | 3.49 | 28 | 10.6 | 10.1 | 76 | 1.24 |
YUA0162 | 57 | 60 | Comp | 27 | 1.69 | 7.57 | 55 | 24.6 | 10.8 | 98 | 2.66 |
YUA0162 | 60 | 63 | Comp | 22 | 2.26 | 12.25 | 44 | 21.6 | 4.9 | 83 | 6.29 |
YUA0162 | 63 | 66 | Comp | 20 | 1.55 | 9.24 | 29 | 24.8 | 4.6 | 106 | 1.28 |
YUA0162 | 66 | 69 | Comp | 16 | 0.81 | 5.60 | 30 | 24.8 | 5.7 | 75 | 0.96 |
YUA0162 | 69 | 72 | Comp | 16 | 0.95 | 3.20 | 17 | 13.7 | 5.1 | 64 | 0.57 |
YUA0162 | 72 | 74 | Comp | 70 | 1.30 | 4.95 | 11 | 99.7 | 8.6 | 125 | 0.81 |
YUA0162 | 74 | 75 | EOH | 14 | 0.27 | 1.54 | 7 | 9.9 | 7.7 | 138 | 0.76 |
YUA0163 | 59 | 60 | EOH | 2 | 0.10 | 0.50 | 70 | 1.0 | 6.1 | 174 | 0.11 |
YUA0164 | 59 | 60 | EOH | 3 | 0.04 | 0.50 | 56 | 0.5 | 8.9 | 269 | 0.12 |
YUA0165 | 56 | 57 | EOH | 3 | 0.28 | 0.28 | 40 | 0.5 | 6.7 | 186 | 0.06 |
YUA0166 | 47 | 48 | EOH | 1 | 0.06 | 0.17 | 35 | 0.4 | 4.6 | 94 | -0.05 |
YUA0167 | 68 | 69 | EOH | 2 | 0.10 | 0.26 | 43 | 0.8 | 2.1 | 92 | 0.05 |
YUA0168 | 62 | 63 | EOH | 14 | 0.21 | 2.62 | 99 | 1.1 | 7.8 | 199 | 0.67 |
YUA0169 | 17 | 18 | EOH | 2 | 0.32 | 1.62 | 4 | 0.8 | 3.5 | 29 | -0.05 |
YUA0170 | 17 | 18 | EOH | 5 | 0.12 | 0.95 | 9 | 0.9 | 2.0 | 20 | 0.05 |
YUA0171 | 20 | 21 | EOH | 3 | 0.35 | 0.70 | 11 | 0.9 | 2.8 | 132 | -0.05 |
YUA0172 | 21 | 22 | EOH | 9 | 0.48 | 0.61 | 6 | 1.0 | 6.8 | 14 | -0.05 |
YUA0173 | 19 | 20 | EOH | 2 | 0.20 | 0.22 | 66 | 1.4 | 2.5 | 52 | -0.05 |
YUA0174 | 41 | 42 | EOH | 5 | 0.78 | 9.50 | 7 | 2.9 | 6.3 | 84 | 0.15 |
YUA0175 | 27 | 28 | EOH | 47 | 0.12 | 0.54 | 24 | 2.1 | 9.2 | 65 | -0.05 |
YUA0176 | 23 | 24 | EOH | 4 | 0.17 | 0.28 | 12 | 1.5 | 1.6 | 26 | -0.05 |
YUA0177 | 28 | 29 | EOH | 2 | 0.09 | 0.25 | 22 | 1.0 | 0.9 | 50 | 0.05 |
YUA0178 | 25 | 26 | EOH | 11 | 0.11 | 0.11 | 9 | 0.5 | 0.6 | 16 | -0.05 |
YUA0179 | 34 | 35 | EOH | 21 | 0.04 | 0.27 | 104 | 0.8 | 9.3 | 155 | 0.17 |
YUA0180 | 35 | 36 | EOH | 2 | 0.05 | 0.17 | 175 | 0.5 | 8.1 | 154 | 0.36 |
YUA0181 | 24 | 27 | Comp | 1 | 0.06 | 0.10 | 23 | 0.4 | 1.6 | 15 | -0.05 |
YUA0181 | 27 | 30 | Comp | 4 | 0.23 | 0.61 | 47 | 2.2 | 4.0 | 65 | 0.14 |
YUA0181 | 30 | 33 | Comp | 3 | 0.15 | 0.46 | 141 | 2.7 | 3.0 | 69 | 0.1 |
YUA0181 | 33 | 36 | Comp | 1 | 0.16 | 1.03 | 211 | 7.1 | 7.0 | 175 | 0.18 |
YUA0181 | 36 | 39 | Comp | 3 | 0.06 | 0.63 | 74 | 2.6 | 5.0 | 123 | 0.09 |
YUA0181 | 39 | 42 | Comp | 3 | 0.11 | 0.61 | 131 | 2.9 | 5.5 | 105 | 0.12 |
YUA0181 | 42 | 45 | Comp | 4 | 0.17 | 0.97 | 176 | 3.1 | 4.1 | 81 | 0.19 |
YUA0181 | 45 | 47 | Comp | 4 | 0.12 | 0.56 | 139 | 3.2 | 4.1 | 83 | 0.1 |
YUA0181 | 47 | 48 | EOH | 2 | 0.13 | 0.65 | 150 | 3.0 | 3.8 | 74 | 0.08 |
YUA0182 | 43 | 44 | EOH | 12 | 0.12 | 0.83 | 299 | 1.2 | 24.7 | 190 | 0.37 |
YUA0183 | 49 | 50 | EOH | 50 | 0.55 | 0.29 | 176 | 0.9 | 7.4 | 199 | 0.07 |
YUA0184 | 25 | 26 | EOH | 3 | 1.88 | 0.19 | 29 | 4.2 | 2.1 | 27 | 0.06 |
YUA0185 | 18 | 21 | Comp | 13 | 0.09 | 0.13 | 21 | 0.8 | 0.7 | 32 | -0.05 |
YUA0185 | 21 | 24 | Comp | 4 | 0.08 | 0.19 | 22 | 1.2 | 1.5 | 30 | 0.05 |
YUA0185 | 24 | 27 | Comp | 3 | 0.25 | 3.52 | 45 | 6.6 | 6.8 | 43 | 0.12 |
YUA0185 | 27 | 30 | Comp | 2 | 0.17 | 3.27 | 117 | 2.2 | 12.9 | 51 | 0.2 |
YUA0185 | 30 | 33 | Comp | 6 | 1.00 | 2.73 | 353 | 1.6 | 10.5 | 333 | 0.13 |
YUA0185 | 33 | 36 | Comp | 17 | 1.08 | 1.02 | 288 | 1.2 | 11.8 | 387 | 0.1 |
YUA0185 | 36 | 39 | Comp | 19 | 0.65 | 0.91 | 236 | 6.5 | 11.7 | 238 | 0.06 |
YUA0185 | 39 | 42 | Comp | 28 | 0.05 | 1.54 | 233 | 1.3 | 12.1 | 254 | 0.08 |
YUA0185 | 42 | 44 | Comp | 10 | 0.15 | 0.83 | 153 | 1.0 | 11.9 | 139 | -0.05 |
YUA0185 | 44 | 45 | EOH | 12 | 0.16 | 1.04 | 156 | 1.2 | 9.0 | 118 | 0.06 |
YUA0186 | 32 | 33 | EOH | 4 | 0.08 | 0.30 | 58 | 1.4 | 1.9 | 50 | -0.05 |
YUA0187 | 77 | 78 | EOH | 2 | 0.16 | 0.44 | 54 | 1.3 | 7.2 | 120 | 0.12 |
Appendix 3: Soil sample results for Au, Sb, and As, relevant to the mineralisation style and reported in this release. Bold values are considered anomalous for the district
Sample ID | Type | Easting (m) | Northing (m) | Height (m) | As (ppm) | Au (ppb) | Sb (ppm) |
J5056 | Soil | 562,602 | 7,674,442 | 58 | 8 | 5 | 1.3 |
J5057 | Soil | 562,600 | 7,674,363 | 53 | 9 | 3 | 2.8 |
J5058 | Soil | 562,604 | 7,674,282 | 55 | 8 | 3 | 3.2 |
J5059 | Soil | 562,565 | 7,674,042 | 51 | 5 | 4 | 1.5 |
J5060 | Soil | 562,604 | 7,674,042 | 50 | 13 | 3 | 10.3 |
J5061 | Soil | 562,644 | 7,674,041 | 49 | 63 | 4 | 26.5 |
J5062 | Soil | 562,683 | 7,674,042 | 48 | 51 | 11 | 18.5 |
J5063 | Soil | 562,722 | 7,674,042 | 48 | 74 | 18 | 27.9 |
J5064 | Soil | 562,763 | 7,674,042 | 46 | 22 | 4 | 16.3 |
J5066 | Soil | 562,804 | 7,674,042 | 47 | 17 | 9 | 4.7 |
J5067 | Soil | 562,841 | 7,674,041 | 42 | 9 | 5 | 2.2 |
J5068 | Soil | 562,883 | 7,674,043 | 38 | 7 | 2 | 1.0 |
J5069 | Soil | 562,803 | 7,673,881 | 40 | 5 | 1 | 0.6 |
J5071 | Soil | 562,762 | 7,673,884 | 39 | 9 | 3 | 1.3 |
J5072 | Soil | 562,724 | 7,673,881 | 40 | 9 | 3 | 4.5 |
J5073 | Soil | 562,685 | 7,673,875 | 41 | 18 | 5 | 23.1 |
J5074 | Soil | 562,643 | 7,673,882 | 45 | 13 | 6 | 3.5 |
J5075 | Soil | 562,603 | 7,673,882 | 46 | 17 | 7 | 7.3 |
J5076 | Soil | 562,564 | 7,673,882 | 54 | 7 | 3 | 4.7 |
J5077 | Soil | 562,522 | 7,673,882 | 59 | 4 | 3 | 1.1 |
J5078 | Soil | 562,483 | 7,673,882 | 62 | 3 | 3 | 0.3 |
J5079 | Soil | 562,443 | 7,673,722 | 51 | 4 | 4 | 5.4 |
J5080 | Soil | 562,483 | 7,673,722 | 51 | 3 | 5 | 3.5 |
J5081 | Soil | 562,523 | 7,673,722 | 47 | 5 | 4 | 3.1 |
J5082 | Soil | 562,564 | 7,673,722 | 48 | 7 | 3 | 3.4 |
J5083 | Soil | 562,604 | 7,673,722 | 48 | 11 | 4 | 7.0 |
J5084 | Soil | 562,637 | 7,673,722 | 45 | 7 | 4 | 2.0 |
J5086 | Soil | 562,683 | 7,673,722 | 46 | 8 | 26 | 1.4 |
J5087 | Soil | 562,723 | 7,673,722 | 44 | 13 | 4 | 2.1 |
J5088 | Soil | 562,757 | 7,673,719 | 45 | 7 | 2 | 0.9 |
J5089 | Soil | 562,764 | 7,673,562 | 46 | 16 | 5 | 6.3 |
J5090 | Soil | 562,724 | 7,673,562 | 45 | 17 | 3 | 10.7 |
J5091 | Soil | 562,683 | 7,673,562 | 51 | 37 | 19 | 19.8 |
J5092 | Soil | 562,644 | 7,673,562 | 56 | 19 | 2 | 11.4 |
J5093 | Soil | 562,603 | 7,673,562 | 54 | 19 | 1 | 17.0 |
J5094 | Soil | 562,563 | 7,673,562 | 52 | 26 | 3 | 33.0 |
J5096 | Soil | 562,523 | 7,673,561 | 55 | 5 | 2 | 3.0 |
J5097 | Soil | 562,524 | 7,673,482 | 55 | 4 | 1 | 1.3 |
J5098 | Soil | 562,564 | 7,673,482 | 55 | 37 | 6 | 15.2 |
J5099 | Soil | 562,603 | 7,673,482 | 53 | 22 | 2 | 18.6 |
J5100 | Soil | 562,643 | 7,673,482 | 46 | 13 | 1 | 8.6 |
J5117 | Soil | 562,684 | 7,673,482 | 43 | 22 | 3 | 9.9 |
J5118 | Soil | 562,722 | 7,673,483 | 41 | 12 | 2 | 5.5 |
J5119 | Soil | 562,764 | 7,673,481 | 38 | 8 | 85 | 2.3 |
J5121 | Soil | 562,724 | 7,673,322 | 36 | 10 | 3 | 2.2 |
J5122 | Soil | 562,684 | 7,673,322 | 41 | 81 | 7 | 20.8 |
J5123 | Soil | 562,644 | 7,673,322 | 42 | 19 | 4 | 19.5 |
J5124 | Soil | 562,604 | 7,673,322 | 41 | 24 | 2 | 9.2 |
J5125 | Soil | 562,562 | 7,673,322 | 43 | 24 | 4 | 33.9 |
J5126 | Soil | 562,523 | 7,673,322 | 41 | 5 | 4 | 1.4 |
J5127 | Soil | 562,523 | 7,673,162 | 47 | 5 | 3 | 1.7 |
J5128 | Soil | 562,564 | 7,673,162 | 47 | 53 | 6 | 37.4 |
J5129 | Soil | 562,604 | 7,673,162 | 45 | 47 | 4 | 21.2 |
J5130 | Soil | 562,643 | 7,673,162 | 44 | 32 | 3 | 14.4 |
J5131 | Soil | 562,683 | 7,673,162 | 42 | 11 | 4 | 4.0 |
J5132 | Soil | 562,723 | 7,673,163 | 41 | 6 | 1 | 1.3 |
J5133 | Soil | 562,764 | 7,673,162 | 42 | 7 | 2 | 0.9 |
J5134 | Soil | 562,721 | 7,673,003 | 40 | 15 | 12 | 3.8 |
J5136 | Soil | 562,682 | 7,672,999 | 42 | 6 | 2 | 1.5 |
J5137 | Soil | 562,643 | 7,673,002 | 45 | 51 | 12 | 23.8 |
J5138 | Soil | 562,603 | 7,673,002 | 46 | 34 | 3 | 48.3 |
J5139 | Soil | 562,563 | 7,673,002 | 48 | 24 | 7 | 18.6 |
J5140 | Soil | 562,523 | 7,673,002 | 47 | 9 | 2 | 4.4 |
J5141 | Soil | 562,524 | 7,672,842 | 51 | 14 | 5 | 11.3 |
J5142 | Soil | 562,563 | 7,672,842 | 50 | 14 | 4 | 7.7 |
J5143 | Soil | 562,603 | 7,672,842 | 49 | 27 | 31 | 21.7 |
J5144 | Soil | 562,639 | 7,672,842 | 50 | 35 | 7 | 10.2 |
J5146 | Soil | 562,683 | 7,672,843 | 47 | 7 | 2 | 1.6 |
J5147 | Soil | 562,643 | 7,672,682 | 46 | 6 | 2 | 0.8 |
J5148 | Soil | 562,603 | 7,672,682 | 49 | 13 | 5 | 1.8 |
J5149 | Soil | 562,564 | 7,672,682 | 50 | 11 | 2 | 2.0 |
J5150 | Soil | 562,524 | 7,672,682 | 49 | 13 | 12 | 4.3 |
J5201 | Soil | 562,563 | 7,674,442 | 61 | 7 | 6 | 1.1 |
J5201 | Soil | 562,563 | 7,674,442 | 61 | 7 | 6 | 1.1 |
J5202 | Soil | 562,564 | 7,674,362 | 53 | 8 | 2 | 3.1 |
J5202 | Soil | 562,564 | 7,674,362 | 53 | 8 | 2 | 3.1 |
J5203 | Soil | 562,563 | 7,674,282 | 52 | 7 | 8 | 2.8 |
J5203 | Soil | 562,563 | 7,674,282 | 52 | 7 | 8 | 2.8 |
J5204 | Soil | 562,602 | 7,674,203 | 50 | 7 | 3 | 8.2 |
J5204 | Soil | 562,602 | 7,674,203 | 50 | 7 | 3 | 8.2 |
J5205 | Soil | 562,602 | 7,674,122 | 44 | 5 | 1 | 2.5 |
J5205 | Soil | 562,602 | 7,674,122 | 44 | 5 | 1 | 2.5 |
J5206 | Soil | 562,644 | 7,674,122 | 45 | 8 | 2 | 5.5 |
J5206 | Soil | 562,644 | 7,674,122 | 45 | 8 | 2 | 5.5 |
J5207 | Soil | 562,684 | 7,674,122 | 49 | 13 | 2 | 6.1 |
J5207 | Soil | 562,684 | 7,674,122 | 49 | 13 | 2 | 6.1 |
J5208 | Soil | 562,724 | 7,674,122 | 47 | 17 | 3 | 7.5 |
J5208 | Soil | 562,724 | 7,674,122 | 47 | 17 | 3 | 7.5 |
J5209 | Soil | 562,763 | 7,674,122 | 46 | 6 | 9 | 5.1 |
J5209 | Soil | 562,763 | 7,674,122 | 46 | 6 | 9 | 5.1 |
J5210 | Soil | 562,805 | 7,674,122 | 47 | 5 | 5 | 2.7 |
J5210 | Soil | 562,805 | 7,674,122 | 47 | 5 | 5 | 2.7 |
J5211 | Soil | 562,844 | 7,674,122 | 44 | 6 | 2 | 1.6 |
J5211 | Soil | 562,844 | 7,674,122 | 44 | 6 | 2 | 1.6 |
J5212 | Soil | 562,844 | 7,673,962 | 38 | 6 | 4 | 0.9 |
J5212 | Soil | 562,844 | 7,673,962 | 38 | 6 | 4 | 0.9 |
J5213 | Soil | 562,803 | 7,673,962 | 37 | 14 | 6 | 1.5 |
J5213 | Soil | 562,803 | 7,673,962 | 37 | 14 | 6 | 1.5 |
J5214 | Soil | 562,762 | 7,673,962 | 43 | 15 | 4 | 5.1 |
J5214 | Soil | 562,762 | 7,673,962 | 43 | 15 | 4 | 5.1 |
J5216 | Soil | 562,723 | 7,673,962 | 41 | 23 | 4 | 5.8 |
J5216 | Soil | 562,723 | 7,673,962 | 41 | 23 | 4 | 5.8 |
J5217 | Soil | 562,684 | 7,673,962 | 44 | 14 | 4 | 12.7 |
J5217 | Soil | 562,684 | 7,673,962 | 44 | 14 | 4 | 12.7 |
J5218 | Soil | 562,643 | 7,673,962 | 50 | 18 | 10 | 10.6 |
J5218 | Soil | 562,643 | 7,673,962 | 50 | 18 | 10 | 10.6 |
J5219 | Soil | 562,604 | 7,673,962 | 48 | 27 | 6 | 27.4 |
J5219 | Soil | 562,604 | 7,673,962 | 48 | 27 | 6 | 27.4 |
J5221 | Soil | 562,563 | 7,673,962 | 46 | 4 | 3 | 1.3 |
J5221 | Soil | 562,563 | 7,673,962 | 46 | 4 | 3 | 1.3 |
J5222 | Soil | 562,522 | 7,673,962 | 50 | 4 | 2 | 0.7 |
J5222 | Soil | 562,522 | 7,673,962 | 50 | 4 | 2 | 0.7 |
J5223 | Soil | 562,444 | 7,673,802 | 67 | 3 | 3 | 0.2 |
J5223 | Soil | 562,444 | 7,673,802 | 67 | 3 | 3 | 0.2 |
J5224 | Soil | 562,483 | 7,673,802 | 58 | 3 | 3 | 0.9 |
J5224 | Soil | 562,483 | 7,673,802 | 58 | 3 | 3 | 0.9 |
J5225 | Soil | 562,523 | 7,673,801 | 57 | 3 | 3 | 1.2 |
J5225 | Soil | 562,523 | 7,673,801 | 57 | 3 | 3 | 1.2 |
J5226 | Soil | 562,563 | 7,673,802 | 50 | 7 | 9 | 3.4 |
J5226 | Soil | 562,563 | 7,673,802 | 50 | 7 | 9 | 3.4 |
J5227 | Soil | 562,603 | 7,673,802 | 48 | 13 | 2 | 15.8 |
J5227 | Soil | 562,603 | 7,673,802 | 48 | 13 | 2 | 15.8 |
J5228 | Soil | 562,643 | 7,673,802 | 41 | 6 | 1 | 1.6 |
J5228 | Soil | 562,643 | 7,673,802 | 41 | 6 | 1 | 1.6 |
J5229 | Soil | 562,683 | 7,673,802 | 46 | 10 | 4 | 2.9 |
J5229 | Soil | 562,683 | 7,673,802 | 46 | 10 | 4 | 2.9 |
J5230 | Soil | 562,724 | 7,673,802 | 45 | 11 | 5 | 2.3 |
J5230 | Soil | 562,724 | 7,673,802 | 45 | 11 | 5 | 2.3 |
J5231 | Soil | 562,762 | 7,673,802 | 41 | 6 | 21 | 0.8 |
J5231 | Soil | 562,762 | 7,673,802 | 41 | 6 | 21 | 0.8 |
J5232 | Soil | 562,803 | 7,673,802 | 39 | 7 | 3 | 1.6 |
J5232 | Soil | 562,803 | 7,673,802 | 39 | 7 | 3 | 1.6 |
J5233 | Soil | 562,724 | 7,673,642 | 46 | 10 | 6 | 2.3 |
J5233 | Soil | 562,724 | 7,673,642 | 46 | 10 | 6 | 2.3 |
J5234 | Soil | 562,684 | 7,673,642 | 46 | 17 | 2 | 4.3 |
J5234 | Soil | 562,684 | 7,673,642 | 46 | 17 | 2 | 4.3 |
J5236 | Soil | 562,644 | 7,673,642 | 53 | 23 | 3 | 29.0 |
J5236 | Soil | 562,644 | 7,673,642 | 53 | 23 | 3 | 29.0 |
J5237 | Soil | 562,602 | 7,673,643 | 47 | 20 | 6 | 17.2 |
J5237 | Soil | 562,602 | 7,673,643 | 47 | 20 | 6 | 17.2 |
J5238 | Soil | 562,565 | 7,673,642 | 45 | 12 | 8 | 7.6 |
J5238 | Soil | 562,565 | 7,673,642 | 45 | 12 | 8 | 7.6 |
J5239 | Soil | 562,523 | 7,673,641 | 49 | 6 | 2 | 8.4 |
J5239 | Soil | 562,523 | 7,673,641 | 49 | 6 | 2 | 8.4 |
J5240 | Soil | 562,484 | 7,673,642 | 55 | 3 | 2 | 2.8 |
J5240 | Soil | 562,484 | 7,673,642 | 55 | 3 | 2 | 2.8 |
J5241 | Soil | 562,443 | 7,673,643 | 64 | 3 | 1 | 3.4 |
J5241 | Soil | 562,443 | 7,673,643 | 64 | 3 | 1 | 3.4 |
J5242 | Soil | 562,525 | 7,673,403 | 41 | 5 | 4 | 3.7 |
J5242 | Soil | 562,525 | 7,673,403 | 41 | 5 | 4 | 3.7 |
J5243 | Soil | 562,563 | 7,673,402 | 47 | 20 | 4 | 21.4 |
J5243 | Soil | 562,563 | 7,673,402 | 47 | 20 | 4 | 21.4 |
J5244 | Soil | 562,604 | 7,673,402 | 47 | 40 | 3 | 21.9 |
J5244 | Soil | 562,604 | 7,673,402 | 47 | 40 | 3 | 21.9 |
J5246 | Soil | 562,643 | 7,673,403 | 44 | 21 | 2 | 17.0 |
J5246 | Soil | 562,643 | 7,673,403 | 44 | 21 | 2 | 17.0 |
J5247 | Soil | 562,682 | 7,673,402 | 40 | 32 | 6 | 24.6 |
J5247 | Soil | 562,682 | 7,673,402 | 40 | 32 | 6 | 24.6 |
J5248 | Soil | 562,723 | 7,673,402 | 39 | 15 | 3 | 5.5 |
J5248 | Soil | 562,723 | 7,673,402 | 39 | 15 | 3 | 5.5 |
J5249 | Soil | 562,722 | 7,673,243 | 42 | 8 | 4 | 1.6 |
J5249 | Soil | 562,722 | 7,673,243 | 42 | 8 | 4 | 1.6 |
J5250 | Soil | 562,684 | 7,673,241 | 41 | 14 | 3 | 5.3 |
J5250 | Soil | 562,684 | 7,673,241 | 41 | 14 | 3 | 5.3 |
J5251 | Soil | 562,644 | 7,673,242 | 45 | 19 | 2 | 5.4 |
J5251 | Soil | 562,644 | 7,673,242 | 45 | 19 | 2 | 5.4 |
J5252 | Soil | 562,604 | 7,673,242 | 39 | 16 | 42 | 10.7 |
J5252 | Soil | 562,604 | 7,673,242 | 39 | 16 | 42 | 10.7 |
J5253 | Soil | 562,563 | 7,673,242 | 45 | 21 | 8 | 25.9 |
J5253 | Soil | 562,563 | 7,673,242 | 45 | 21 | 8 | 25.9 |
J5254 | Soil | 562,523 | 7,673,242 | 48 | 4 | 2 | 1.2 |
J5254 | Soil | 562,523 | 7,673,242 | 48 | 4 | 2 | 1.2 |
J5255 | Soil | 562,524 | 7,673,082 | 50 | 27 | 4 | 42.9 |
J5255 | Soil | 562,524 | 7,673,082 | 50 | 27 | 4 | 42.9 |
J5256 | Soil | 562,563 | 7,673,083 | 48 | 21 | 2 | 15.2 |
J5256 | Soil | 562,563 | 7,673,083 | 48 | 21 | 2 | 15.2 |
J5257 | Soil | 562,603 | 7,673,081 | 46 | 38 | 6 | 39.2 |
J5257 | Soil | 562,603 | 7,673,081 | 46 | 38 | 6 | 39.2 |
J5258 | Soil | 562,644 | 7,673,082 | 41 | 33 | 5 | 21.6 |
J5258 | Soil | 562,644 | 7,673,082 | 41 | 33 | 5 | 21.6 |
J5259 | Soil | 562,684 | 7,673,082 | 40 | 7 | 2 | 1.9 |
J5259 | Soil | 562,684 | 7,673,082 | 40 | 7 | 2 | 1.9 |
J5260 | Soil | 562,722 | 7,673,081 | 40 | 8 | 2 | 3.7 |
J5260 | Soil | 562,722 | 7,673,081 | 40 | 8 | 2 | 3.7 |
J5261 | Soil | 562,764 | 7,673,083 | 39 | 6 | 1 | 0.8 |
J5261 | Soil | 562,764 | 7,673,083 | 39 | 6 | 1 | 0.8 |
J5262 | Soil | 562,763 | 7,672,921 | 36 | 6 | 3 | 0.9 |
J5262 | Soil | 562,763 | 7,672,921 | 36 | 6 | 3 | 0.9 |
J5263 | Soil | 562,721 | 7,672,920 | 39 | 17 | 11 | 9.8 |
J5263 | Soil | 562,721 | 7,672,920 | 39 | 17 | 11 | 9.8 |
J5264 | Soil | 562,683 | 7,672,922 | 40 | 9 | 1 | 3.1 |
J5264 | Soil | 562,683 | 7,672,922 | 40 | 9 | 1 | 3.1 |
J5266 | Soil | 562,643 | 7,672,922 | 41 | 24 | 2 | 11.2 |
J5266 | Soil | 562,643 | 7,672,922 | 41 | 24 | 2 | 11.2 |
J5267 | Soil | 562,603 | 7,672,921 | 43 | 60 | 4 | 35.0 |
J5267 | Soil | 562,603 | 7,672,921 | 43 | 60 | 4 | 35.0 |
J5268 | Soil | 562,563 | 7,672,921 | 45 | 31 | 4 | 32.8 |
J5268 | Soil | 562,563 | 7,672,921 | 45 | 31 | 4 | 32.8 |
J5269 | Soil | 562,524 | 7,672,922 | 47 | 28 | 6 | 7.0 |
J5269 | Soil | 562,524 | 7,672,922 | 47 | 28 | 6 | 7.0 |
J5271 | Soil | 562,523 | 7,672,762 | 52 | 12 | 4 | 4.5 |
J5271 | Soil | 562,523 | 7,672,762 | 52 | 12 | 4 | 4.5 |
J5272 | Soil | 562,563 | 7,672,760 | 47 | 12 | 2 | 2.4 |
J5272 | Soil | 562,563 | 7,672,760 | 47 | 12 | 2 | 2.4 |
J5273 | Soil | 562,603 | 7,672,762 | 47 | 14 | 2 | 3.1 |
J5273 | Soil | 562,603 | 7,672,762 | 47 | 14 | 2 | 3.1 |
J5274 | Soil | 562,644 | 7,672,762 | 46 | 79 | 22 | 22.7 |
J5274 | Soil | 562,644 | 7,672,762 | 46 | 79 | 22 | 22.7 |
J5275 | Soil | 562,684 | 7,672,762 | 46 | 13 | 2 | 3.2 |
J5275 | Soil | 562,684 | 7,672,762 | 46 | 13 | 2 | 3.2 |
J5276 | Soil | 562,674 | 7,672,600 | 42 | 12 | 5 | 2.8 |
J5276 | Soil | 562,674 | 7,672,600 | 42 | 12 | 5 | 2.8 |
J5277 | Soil | 562,643 | 7,672,602 | 41 | 7 | 2 | 0.9 |
J5277 | Soil | 562,643 | 7,672,602 | 41 | 7 | 2 | 0.9 |
J5278 | Soil | 562,602 | 7,672,602 | 43 | 13 | 6 | 1.8 |
J5278 | Soil | 562,602 | 7,672,602 | 43 | 13 | 6 | 1.8 |
J5279 | Soil | 562,564 | 7,672,602 | 46 | 12 | 2 | 1.4 |
J5279 | Soil | 562,564 | 7,672,602 | 46 | 12 | 2 | 1.4 |
J5280 | Soil | 562,524 | 7,672,602 | 48 | 17 | 10 | 3.7 |
J5280 | Soil | 562,524 | 7,672,602 | 48 | 17 | 10 | 3.7 |
J5281 | Soil | 562,522 | 7,672,442 | 46 | 7 | 3 | 1.0 |
J5281 | Soil | 562,522 | 7,672,442 | 46 | 7 | 3 | 1.0 |
J5282 | Soil | 562,564 | 7,672,442 | 44 | 10 | 3 | 0.8 |
J5282 | Soil | 562,564 | 7,672,442 | 44 | 10 | 3 | 0.8 |
J5283 | Soil | 562,603 | 7,672,442 | 42 | 12 | 4 | 1.3 |
J5283 | Soil | 562,603 | 7,672,442 | 42 | 12 | 4 | 1.3 |
J5284 | Soil | 562,568 | 7,672,282 | 44 | 8 | 4 | 0.7 |
J5284 | Soil | 562,568 | 7,672,282 | 44 | 8 | 4 | 0.7 |
J5286 | Soil | 562,523 | 7,672,282 | 46 | 8 | 2 | 1.1 |
J5286 | Soil | 562,523 | 7,672,282 | 46 | 8 | 2 | 1.1 |
J5301 | Soil | 562,523 | 7,672,522 | 51 | 8 | 15 | 0.7 |
J5302 | Soil | 562,564 | 7,672,522 | 49 | 16 | 6 | 1.4 |
J5303 | Soil | 562,602 | 7,672,522 | 44 | 8 | 2 | 1.3 |
J5304 | Soil | 562,595 | 7,672,362 | 43 | 9 | 2 | 0.9 |
J5305 | Soil | 562,561 | 7,672,362 | 46 | 6 | 1 | 0.6 |
J5306 | Soil | 562,522 | 7,672,362 | 50 | 11 | 3 | 1.7 |
Appendix 4: Rock sample results for Au, Sb, and As, relevant to the mineralisation style and reported in this release. Bold values are considered anomalous for the district
Sample ID | Type | Easting (m) | Northing (m) | Height (m) | As (ppm) | Au (ppb) | Sb (ppm) |
R07957 | Rock | 562,577 | 7,672,876 | 50 | 39 | 3 | 15 |
R07958 | Rock | 562,566 | 7,673,302 | 34 | 156 | 2 | 2,150 |
R07959 | Rock | 562,577 | 7,673,302 | 35 | 168 | 3 | 673 |
R07960 | Rock | 562,595 | 7,673,103 | 46 | 12 | 1 | 16 |
R07961 | Rock | 562,557 | 7,673,094 | 48 | 273 | 4 | 710 |
R07962 | Rock | 562,529 | 7,673,094 | 46 | 219 | 4 | 1,650 |
R07963 | Rock | 562,618 | 7,673,025 | 46 | 651 | 11 | 1,230 |
R07964 | Rock | 562,564 | 7,673,540 | 47 | 50 | 4 | 51 |
R07965 | Rock | 562,644 | 7,674,051 | 45 | 1,120 | 4 | 241 |
R07967 | Rock | 562,683 | 7,674,027 | 47 | 12 | 1 | 101 |
R07968 | Rock | 562,788 | 7,674,045 | 50 | 30 | 1 | 88 |
R07970 | Rock | 562,718 | 7,674,051 | 53 | 240 | 2 | 226 |
JORC Code, 2012 Edition – Table 1
Section 1: Sampling Techniques and Data
(Criteria listed in the preceding section also apply to this section)
Criteria | JORC Code explanation | Commentary |
Sampling techniques | - Nature and quality of sampling (e.g., cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling.
- Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used.
- Aspects of the determination of mineralisation that are Material to the Public Report.
- In cases where ‘industry standard’ work has been done this would be relatively simple (e.g., ‘reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay’). In other cases, more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (e.g., submarine nodules) may warrant disclosure of detailed information.
| - Balla Balla AC samples were speared from 1 m sample piles into 3 m composites. Composite length was reduced at end of hole to accommodate a final one metre end of hole sample.
- Samples are approximately 2 – 3 kg, and pulverised in full
- Speared composite samples were analysed for gold using a 50 g fire assay.
- End of hole samples were analysed for gold, platinum and palladium using a 50 g PGM-ICP24 assay and for multi-elements using a 0.25 g ME-MS61 assay
- Sherlock Crossing rock chips samples were collected by grab sampling 1 – 3 kg of material. Sample sites were selected to be representative of the lithology sampled, and the same sampling technique was employed at each sample site where possible. Samples are pulverised in full and analysed for gold using a 50 g fire assay (Au-ICP22) and for multi-elements using a 0.25 g ME-MS61 assay
- Sherlock Crossing soil samples of ~200 g were collected from small pits 10 cm – 40 cm in depth and sieved to <80# mesh. A 25 g aliquot was digested via aqua regia (AuME-TL43)
|
Drilling techniques | - Drill type (e.g., core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details (e.g., core diameter, triple or standard tube, depth of diamond tails, face-sampling bit, or other type, whether core is oriented and if so, by what method, etc).
| - Balla Balla AC drilling was completed by Wallis Drilling, using a Mantis 200 drill rig with NQ sized drill rods
|
Drill sample recovery | - Method of recording and assessing core and chip sample recoveries and results assessed.
- Measures taken to maximise sample recovery and ensure representative nature of the samples.
- Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material.
| - Sample recoveries were estimated from sample piles. Records were made of sample quality, including contamination and wetness.
- The rig utilises a cyclone to ensure all material is captured in metre intervals, with dust suppression to retain fines. The cyclone was regularly cleaned to minimise sample contamination
- No relationship between sample recovery or contamination and grade is recognised.
|
Logging | - Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies.
- Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography.
- The total length and percentage of the relevant intersections logged.
| - AC chips were logged for qualitative and quantitative properties including interpreted lithology, alteration and mineralisation, magsus, and sample properties. Chips and pieces of core were photographed and stored for future test work. All one metre intervals are logged.
- Chips were not analysed for geotechnical or metallurgical properties, and this preliminary program will not be part of a Mineral Resource estimation
- Rock chip samples are geologically logged with quantitative and qualitative data collected including a description of lithology, vein type and vein densities, and alteration.
|
Sub-sampling techniques and sample preparation | - If core, whether cut or sawn and whether quarter, half or all core taken.
- If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry.
- For all sample types, the nature, quality, and appropriateness of the sample preparation technique.
- Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples.
- Measures taken to ensure that the sampling is representative of the in-situ material collected, including for instance results for field duplicate/second-half sampling.
- Whether sample sizes are appropriate to the grain size of the material being sampled.
| - Balla Balla AC samples were speared from one metre sample piles into three metre composites.
- Spearing AC samples from piles on the ground is appropriate for the early exploration phase. Spearing is completed with a custom made pvc spear, held parallel to the ground to avoid contamination, and speared into the centre of the sample pile to best represent the entire metre drilled. Equal aliquots are combined into a three-metre composite for assay.
- Duplicate samples were collected for every 1 in 25 samples to check for repeatability.
- The sampling techniques and sample sizes are considered appropriate for the style of mineralisation.
- Rock samples are collected to best represent the material sampled across geological features.
|
Quality of assay data and laboratory tests | - The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total.
- For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc.
- Nature of quality control procedures adopted (e.g., standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (if lack of bias) and precision have been established.
| - AC sampling and analysis is considered appropriate for early exploration and the style of mineralisation tested. QAQC includes 2 CRM standards, 2 blanks, and 4 field duplicates per 100 samples.
- The rock chip sample assay methodology is considered appropriate for the style of mineralisation tested. The method includes inserting 2 CRM standards and 2 blanks per 100 samples or at least one of each per sample submission.
- The soil sample assay methodology has low level detection for gold and multi-elements and is considered appropriate for soil geochemistry for outcropping or near surface mineralisation. The method includes insertion of at least 2 blanks 2 CRM standards and 4 field duplicates per 100 samples.
- No QAQC issues were detected for Au or ME performance, with CRM performance passing review and no bias detected.
|
Verification of sampling and assaying | - The verification of significant intersections by either independent or alternative company personnel.
- The use of twinned holes.
- Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols.
- Discuss any adjustment to assay data.
| - Primary data was collected in the field using Geobank for Field Teams 24.0, which was then forwarded to the database manager email for upload to the Geobank (v2025.0) database, buffered through a validation portal that ensures code and primary record compliance. Geobank is a front-end UX/UI tender software platform (developed and sold by Micromine) attached to a SQL v15.1 server.
- Assay data was loaded from lab certificates received from the registered laboratory by an internal database manager or external database consultant, and industry-standard audit trails and chain-of-custody was adhered to.
- Verification included checking the data against original logs and utilising laboratory certificates.
- No adjustments of the assay data were made.
|
Location of data points | - Accuracy and quality of surveys used to locate drill holes (collar and down-hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation.
- Specification of the grid system used.
- Quality and adequacy of topographic control.
| - All surface sample locations were recorded by hand-held GPS using the GDA 2020 zone 50 coordinate system.
- AC holes are surveyed at the start of hole using a handheld compass and clino on the rig mast. There are no downhole surveys completed due to the shallow nature of drilling.
- Topographic control at Balla Balla is from SRTM data, which is of sufficient quality for the relatively flat project terrain
|
Data spacing and distribution | - Data spacing for reporting of Exploration Results.
- Whether the data spacing, and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied.
- Whether sample compositing has been applied.
| - AC holes are spaced at 50 m, on lines spaced between 640 m and 2.8 km. This spacing is not sufficient to derive any geological or grade continuity. Samples are composited to 3 m intervals.
- Limited rock samples taken are indicative of potential grade tenor. These do not represent or imply any continuity or scale potential.
- Soil samples were taken on a nominal grid of 40 m by 80 m orientated to be perpendicular to the interpreted strike of the system.
|
Orientation of data in relation to geological structure | - Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type.
- If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material.
| - AC drill lines were designed to be perpendicular to most structures and stratigraphy trends. AC holes were angled to the southeast, which is assuming a vertical or northwest dip to features. Drilling intersected lithological contacts and structures as anticipated, although it is at this stage unknown if other orientated structures are present.
- The soil sample grid was orientated to best intersect the lithological and structural trends at right angles.
- Rock samples were taken across features with geological data recorded to best reflect unbiased sampling of possible mineralised structures.
|
Sample security | - The measures taken to ensure sample security.
| - All samples are stored and managed on site by internal staff. Samples are then transported by reputable companies to a registered laboratory where they are stored in a locked facility before being tracked and processed through the preparation and analysis system at the laboratory.
|
Audits or reviews | - The results of any audits or reviews of sampling techniques and data.
| - No audits have been undertaken.
|
Section 2: Reporting of Exploration Results
(Criteria listed in the preceding section also apply to this section)
Criteria | JORC Code explanation | Commentary |
Mineral tenement and land tenure status | - Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings.
- The security of the tenure held at the time of reporting along with any known impediments to obtaining a license to operate in the area.
| - The Balla Balla project is located on tenements E47/4703 and E47/4295. E47/4703 is held by SQM under the Harding Battery Metals JV, with Novo retaining a 25% interest in the tenement and 100% of the gold, silver, PGE, copper, lead and zinc mineral rights. E47/4295 is held by Meentheena Gold Pty Ltd, a wholly owned subsidiary of Novo.
- The drilling area falls within the Kariyarra Native Title claim. Novo have a tenement wide access agreement in place with Kariyarra and completed heritage surveys to allow AC drilling.
- Sherlock Crossing is located on tenement E47/3825, held by Karratha Gold Pty Ltd, a wholly owned subsidiary of Novo. It falls within the Ngarluma/Yindjibarndi Native Title Claim and is managed by the Ngarluma Aboriginal Corporation. Novo have an access agreement in place with Ngarluma and have completed a heritage survey to facilitate drilling.
- The tenements are currently in good standing and there are no known impediments.
|
Exploration done by other parties | - Acknowledgment and appraisal of exploration by other parties.
| - Balla Balla:
- Australia Inland Exploration and Esso Exploration conducted airborne and ground magnetics, an IP survey, diamond drilling, and thin section petrography targeting massive nickel and copper in the Sherlock Intrusion. The 1975 annual report concludes that any additional work on the tenement would only be justified if a new effective geophysical tool emerged
- Esso Exploration targeted the area in 1980 and 1981 with an additional aeromagnetic survey, an EM survey and RAB drilling. The RAB program consisted of 75 holes for a total of 1,535 m across the project area. All these targeted geophysical anomalies identified across the surveys conducted. Results were broadly disappointing with peak values of 101 ppm Ni, 196 ppm Cu, 127 ppm Zn, 0.5 ppm Ag, 115 ppm W, 92 ppm Pb and 0.05 ppm Au.
- Previous surface sampling was completed over the Ramquarry prospect in a JV between Gascoyne Gold, Dalrymple Resources and Sons of Gwalia in the 1997 to 1998 field season. 22 rock chip samples were taken, with results yielding no gold or base metal anomalies
- Golden State Mining in 2020 targeted VMS, shear hosted gold and to a lesser extent Ni-Cu sulphides. Results were broadly uninspiring with a peak Au value of 0.18 ppm Au
- Sherlock Crossing:
- Aarex 1997 (A53516 – A49869) collected thirty-five samples from outcrop or from the dump surrounding the main historical excavation at the Clarke Mine. The highest sample result was 84.8 g/t gold which averaged 68.5 g/t over four assays.
- Ascent Mining 2002 (A66185) collected twenty-one rock chip samples from Sherlock Crossing, located at the site of the historical Clarkes antimony mine, returning up to 98.8 g/t Au and 0.83% antimony
- Ourwest Corp 2007 (A76553) collected eleven rock chip samples which gave peak results of 3.78 g/t Au and 1390 ppm Sb.
- No other known work of relevance has been undertaken by other parties.
|
Geology | - Deposit type, geological setting, and style of mineralisation.
| - The mineralisation style at Balla Balla is unknown. Historical work focussed largely on VMS or shear hosted mineralisation. Results in this release suggest hydrothermal alteration related to shear hosted mineralisation.
- Sherlock Crossing is an orogenic narrow and high-grade vein hosted system, within ultramafics.
|
Drill hole Information | - A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes, including Easting and northing of the drill hole collar, Elevation or RL (Reduced Level – elevation above sea level in metres) of the drill hole collar, dip and azimuth of the hole, down hole length and interception depth plus hole length.
- If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case.
| - Collar details of all aircore holes, significant intercepts for gold mineralisation, and all multi-element data is provided for selected elements in Appendices
- All rock sample and soil sample results are reported in Appendices, listing all significant multi-elements.
|
Data aggregation methods | - In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (e.g., cutting of high grades) and cut-off grades are usually Material and should be stated.
- Where aggregate intercepts incorporate short lengths of high-grade results and longer lengths of low-grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail.
- The assumptions used for any reporting of metal equivalent values should be clearly stated.
| - Results from the AC program are low level. No weighted average or top cuts are applied. Significant intercepts are reported to a 10 ppb cut off, including 3 m of internal waste. Higher-grade results are reported to a 30 ppb cut off, and are higher-grade for the purpose of domaining zones of mineralisation only
|
Relationship between mineralisation widths and intercept lengths | - These relationships are particularly important in the reporting of Exploration Results.
- If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported.
- If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (e.g., ‘down hole length, true width not known’).
| - True orientation of possible mineralisation is currently unknown. The AC drilling was orientated to be perpendicular as best as practical to potential structures. Only down hole lengths of mineralisation are reported here.
- Rock sample results are indicative in nature and, whilst representatively sampling the target lithology, do not contain any width or length information other than a qualitative description of the target.
|
Diagrams | - Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported. These should include but not be limited to a plan view of drill hole collar locations and appropriate sectional views.
| - Refer to the body of the release for appropriate maps and diagrams.
|
Balanced reporting | - Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be practiced to avoid misleading reporting of Exploration Results.
| - Due to the large number of downhole gold assay results, not all results are reported in Appendix 2. All significant results greater than 10 ppb are listed, including any higher-grade where intersected.
- The full multi element suite comprises 50 elements. Not all elements are reported in Appendix 3, but a selection relevant to the mineralisation style is reported. For these elements, all end of hole and down hole intervals are listed.
- All rock sample and soil sample results are reported.
|
Other substantive exploration data | - Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples – size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances.
| |
Further work | - The nature and scale of planned further work (e.g., tests for lateral extensions or depth extensions or large-scale step-out drilling).
- Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive.
| - Refer to the body of the release.
- Further hyperspectral work and geochemical analysis will be conducted on selected material for Balla Balla, to determine whether alteration can vector towards a mineralisation system.
- Novo intends to complete a ~ 1,000 m maiden RC drilling program at the Sherlock Crossing Au-Sb project in H2 2025.
|
No Section 3 or 4 report as no Mineral Resources or Ore Reserves are reported in this Appendix
Figures accompanying this announcement are available at:
https://www.globenewswire.com/NewsRoom/AttachmentNg/94110a26-5abd-4fe0-a0e9-1c28d63bd0bd
https://www.globenewswire.com/NewsRoom/AttachmentNg/a1f5fce0-a78c-4d1a-b690-c8f2f7b89dc8
https://www.globenewswire.com/NewsRoom/AttachmentNg/158a2d37-41b3-4c85-a9d0-1dbf5743c1cd
https://www.globenewswire.com/NewsRoom/AttachmentNg/dabcfd43-a3fc-4104-89fd-cb36372a28a8
https://www.globenewswire.com/NewsRoom/AttachmentNg/b09dfc62-4aa5-4bc7-b1d4-21f4238dca49
https://www.globenewswire.com/NewsRoom/AttachmentNg/d160d450-8422-4c61-9dd2-9e4dd89a3aba



Figure 1
Novo Tenure showing the Egina Gold Camp, Balla Balla Gold Project, and gold prospects.
Figure 2
AC collar locations on interpreted regional geology and structure
Figure 3
AC collar locations over regional geological interpretation and airborne magnetics, showing maximum downhole gold values
Figure 4
Sherlock Crossing, showing extended soil anomaly > 15 ppm Sb to the SW of the proposed first pass drilling area at the Clarke Mine(2)
Figure 5
Main prospects of the Tabba Tabba Shear Corridor
Property Map
Property Map
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