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Trigg Minerals Limited (ASX: TMG) ("Trigg" or the "Company") is pleased to announce it has signed a binding purchase agreement (Sale Agreement) with private company Anchor Resources Pty Limited (Anchor Resources), to acquire the Achilles Antimony Project (Achilles) in northern New South Wales (Figure 1).
HIGHLIGHTS
- Trigg signs purchase agreement to acquire the 100% of the Achilles project which contains the globally significant high-grade and high-tonnage Wild Cattle Creek (WCC) Antimony Deposit.
- The WCC deposit is Australia highest grade undeveloped Antimony deposit and ranks among the highest-grade antimony deposits globally1.
- Significant intersections recorded by historical owners of the project include (refer to Table 2 for full results):
- 10.7m at 14.24% Sb
- 18.7m at 4.5% Sb from including 5.2m at G.8% Sb
- 10.8m at G.28% Sb
- 51.2m at 1.7% Sb including 5.5m at 4.8% Sb
- 22.5m at 3.G% Sb
- 12m at 4.3% Sb
- 10m at 5.1% Sb
- The WCC deposit is the second-largest antimony deposit1 in New South Wales, after Hillgrove, with a resource of 610 kt at 2.56% Sb, containing 15,600 tonnes of antimony. This estimate is based on a high cut-off grade of 1%, reported in accordance with JORC 2012 standards.
- Numerous ultra-high-grade drill intersections grading up to 14.45% Sb have been confirmed beyond the existing JORC resource indicating significant resource upgrades.
- The deposit is enriched from surface and open down plunge hosted by an 6km long largely untested structure.
- Historical metallurgy showed ultra-high antimony recoveries of over 95% are achievable from the WCC deposit through a low-cost conventional milling and flotation technique.
- Trigg post completion will progress further exploration for resource expansion at the WCC deposit while simultaneously advancing it’s 100% owned Taylors Arm antimony project which contains Australia’s highest ever recorded antimony grade at 63% Sb.
- 100% non-cash transaction allows Trigg to preserve its healthy cash balance for value adding exploration.
The Achilles Project hosts the globally significant high grade and high tonnage Wild Cattle Creek antimony deposit, with a JORC 2012-compliant Mineral Resource Estimate (MRE) of 610,000 tonnes at 2.56% Sb, containing 15,600 tonnes of antimony (Indicated and Inferred categories). In addition to antimony, the deposit is enriched with tungsten and gold.
Discovered in the 1890s, the project has historically produced antimony ore during several periods of operation since then, with grades up to 46% Sb reported. Anchor Resources completed the most recent work on the project from 2005 to 2016 when it completed 23 drill holes, two resource estimation studies, orientation soil geochemistry, water and noise monitoring surveys, and sponsored university research into the genesis of the Wild Cattle Creek deposit.
Trigg Minerals Executive Chair Timothy Morrison said, "Acquiring the Achilles Project, including the Wild Cattle Creek antimony deposit, is a significant bolstering of our existing portfolio and provides Trigg Minerals with an advanced project with a JORC resource and plenty of exploration upside in and around the resource. Adding to our recent acquisitions of the Taylors Arms and Spartan antimony projects, we expect Achilles to be our flagship, given its advanced state. This acquisition positions Trigg as a globally significant player in the rush to secure Antinomy supply"
Figure 1: Achilles Antimony Project (EL 6388) - location and tenement with respect to NSW and other recent acquisitions (Taylors Arm and Spartan Antimony Projects) by Trigg.
PROJECT OVERVIEW
The Achilles exploration licence (EL 6388) is 40km west of Coffs Harbour, northeast New South Wales and ~11km north of Dorrigo. The Project contains the Wild Cattle Creek antimony deposit, Australia's second-largest antimony deposit after Hillgrove2 in New South Wales, with the potential for further significant expansion through ongoing exploration.
Geology
The Wild Cattle Creek deposit is in the Coffs Harbour Block of the New England Orogen, within a Late Carboniferous turbidite sequence dominated by siltstone (the Brooklana Beds). These sediments have undergone multiple deformations, regional metamorphism (up to biotite grade), and granitoid intrusions. The block is interpreted as an accretionary prism with subduction-related metamorphism dated at 318 ± 8 Ma. Mineralisation at Wild Cattle Creek is like the nearby Hillgrove antimony-gold deposit, located 80 km to the west-southwest and currently held by Larvotto Resources (ASX: LRV). Wild Cattle Creek is one of approximately 235 antimony occurrences in the New England region of New South Wales.
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This article includes content from Trigg Minerals Limited, licensed for the purpose of publishing on Investing News Australia. This article does not constitute financial product advice. It is your responsibility to perform proper due diligence before acting upon any information provided here. Please refer to our full disclaimer here.
High grade Massive Sulphide Intercepts Confirmed at Oval
HIGHLIGHTS:
- OVD027 confirms the continution of high grade massive sulphide from OVD0211 with an intercept of 6.1 metres of 4.16% Cu, 3.51% Ni, 0.G3g/t E3, and 0.13% Co from G8.2 metres encountered between broader high grade zones of:
- A dense disseminated intercept - 26.2 metres of 0.44% Cu, 0.52% Ni, 0.12g/t E3, and 0.03% Co from 72.0 metres and
- A net textured intercept - 15.3 metres of 1.15% Cu, 0.79% Ni, 0.35g/t E3, and 0.04% Co from 104.3 metres;
- A high grade broad intersection is confirmed at the central part of the Oval area by OVD026. It includes a massive sulphide intercept in hole OVD026 of 1.8 metres of 3.21% Cu, 3.32% Ni, 0.6Gg/t E3, and 0.14% Co from 105.0 metres within broader mineralisation of:
- 19.8 metres of 1.23% Cu, 0.98% Ni, 0.36g/t E3, and 0.05% Co from 91.2 metres.
OVD026 is located 100 metres northwest of the previously announced 8.8 metres of massive sulphide identified in drillhole OVD021.
On completion of the Phase 2 exploration work and receipt of all assays, Managing Director Gan-Ochir Zunduisuren, commented:“The 2024 Phase 1 and 2 drilling and exploration programs have confirmed the broad presence of high-grade mineralisation in the Oval gabbroic intrusion. The grades intercepted in some of the drillholes are exceptional and may be indicative of broader potential over a larger area, given Oval is a greenfields discovery.
The 2025 exploration program will focus on obtaining information on the size/metal content potential of the Oval Cu-Ni-PGE mineral system as well as targeting the possible deeper magmatic sources at Oval. Broader exploration is also planned at potential extensions of Oval and nearby look-a-like prospects. We look forward to updating shareholders on progress, with drilling expected to commence in around 8 weeks”.
Summary of Phase 2 exploration drilling at Oval Cu-Ni-PGE project
The Company’s recent drilling work has predominantly focused on finding high-grade mineralisation in the olivine-amphibole gabbro at the Oval project. The multiple intercepts of massive sulphide mineralisation with different ratios of metal contents throughout the Oval gabbroic intrusion is highly encouraging for the presence of one or more deeper sources of high grade mineralisation in the opinion of ABM.
Figure 1. Plan view of drillhole locations on high resolution magnetics map (RTP)
Drillhole OVD02c
Drillhole OVD026 was designed to test the Down-Hole Electromagnetic (DHEM) conductor plate identified as OVD007_L2_B (reinterpretation of OVD007_L2_A2 by Southern Geoscience Consultants), which exhibits a conductance of 1,000 siemens. The drilling intersected a total of 1G.8 metres of mineralisation with 1.23% Cu, 0.G8% Ni, 0.36g/t E3, and 0.05% Co from G1.2 metres including;
- 4.8 metres of @ 0.45% Cu, 0.43% of Ni, 0.14g/t E3, and 0.02% Co of dense disseminated mineralised gabbro from 91.2 metres,
- 6.6 metres of @ 1.56% Cu, 0.G0% Ni, 0.50g/t E3, and 0.04% Co of net textured mineralisation from G6.0 metres,
- 2.4 metres of @ 1.52% Cu, 1.3G% Ni, 0.43g/t E3, and 0.07% Co of semi massive sulphide mineralisation from 102.6 metres,
- 1.8 metres of @ 3.21% Cu, 3.32% Ni, 0.6Gg/t E3, and 0.14% Co of massive sulphide mineralisation from 105.0 metres, and
- 4.2 metres of @ 0.57% Cu, 0.45% of Ni, 0.21g/t E3, and 0.02% Co of dense disseminated mineralised gabbro from 106.9 metres (Table 1 provides a detailed breakdown of mineralisation intervals).
OVD026 is located in the Oval area, which is approximately 100 metres northwest of the previous intersection identified in drillhole OVD0213. This intercept may represent an extension of the known massive sulphide mineralisation in the Oval area and highlights the potential for further expansion of massive sulphide zones within the broader prospect area (Figures 1 and 3).
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This article includes content from Asian Battery Metals PLC, licensed for the purpose of publishing on Investing News Australia. This article does not constitute financial product advice. It is your responsibility to perform proper due diligence before acting upon any information provided here. Please refer to our full disclaimer here.
