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Augustus Minerals Limited (the Company) refers to the announcement dated 7 June 2024 titled “Minnie Springs High Grade Cu-Mo Porphyry Targeting” (Announcement).
The Company wishes to update the Announcement adding information in respect to Figure 1. Enclosed with this cover page is the updated announcement.
Authorised by the Board of Augustus Minerals Limited.
Augustus Minerals (ASX: AUG; “Augustus” or the “Company”) is pleased to provide an update on geological modelling of mineralisation and alteration mapping following recent RC drilling and reprocessing of historic IP survey data for the Minnie Springs Copper (Cu)-Molybdenum (Mo) project in the Gascoyne Region.
- Augustus Minerals has conducted re-processing of historic Induced Polarisation (IP) geophysics at the Minnie Springs Cu-Mo porphyry project which highlights the potential for near surface extensions to existing Mo mineralisation.
- Potential identified for higher grade Cu and Mo zones at depth below “tilted” porphyry model.
- Cu mineralised quartz veins drilled by Augustus in the 2024 RC program over the eastern part of the prospect may be “smoke” remobilized from higher grade zones at depth by shearing related to the regional Minga Bar fault system.
- Previous drilling at Minnie Springs intersected mineralisation, geology and alteration halo consistent with the zoning of a large porphyry copper / molybdenum system.
- Two holes with EIS funding planned to test for the higher-grade zones at depth.
Andrew Ford, GM Exploration
“Modelling of the Minnie Springs system in an integrated manner by incorporating recent drilling, alteration mapping and geophysics has highlighted both potential extensions to existing near surface Mo rich zones, as well as the potential for higher grade Cu-Mo zones at depth”.
Minnie Springs
Minnie Springs hosts porphyry related Cu-Mo mineralisation that was previously drilled by Equatorial Mining and Catalyst Metals. A molybdenum Exploration Target has previously been defined by SRK Consulting for the historic drilling area comprised of between 12 - 84Mt as outlined below (Table 1 and Figure 2)1. Clarifying Statement: The potential quantity and grade of the exploration target is conceptual in nature, there has been insufficient exploration to estimate a Mineral Resources, and it is uncertain if further exploration will result in the estimation of a Mineral Resource.
Table 1. Exploration target size estimate for Minnie Springs Molybdenum depositNote: Based on ~300 ppm Mo cut-off at 100% recovery.
The recently completed 3,070m RC drilling program that infilled around hole MSRC012 drilled last year (18m @ 0.37% Cu and 9.7 g/t Ag from 94m downhole, and 16m @ 0.38% Cu and 19.4g/t Ag from 121m downhole2) and tested the northern half of the 2km long copper-in soil anomaly continued to extend the footprint of Cu anomalism. Assays from this program >0.1% Cu are Listed in Table 2 below; collar details are listed in Table 3.
The RC drilling has confirmed strong Cu anomalism within quartz veins over a strike length of greater than 3km beneath the strong Cu-in-soils anomaly (Figure 2). The association of the copper with the quartz veins with moderate to low levels of pyrite (no chargeability IP response) suggest structural remobilisation from a deeper copper source. Shearing within the Cu zone increases significantly as it approaches the major northwest trending Minga Bar Fault system; this is supported by a marked increase in water intersected within the RC drilling within the easternmost holes.
As discussed above, the Mo rich core of the system is located southwest of the Cu anomaly which implies that the system is tilted to the east, exposing the Mo rich zone which is usually seen deeper within the porphyry than the Cu zone.
Geophysics
Southern Geoscience Consultants (SGC) reprocessed the two IP Surveys conducted by Equatorial Minerals in 1997. A gradient array survey was conducted over both the Mo and Cu zones, highlighting elevated chargeability over the Mo rich zone, with no significant chargeability over the Cu-in-soil anomaly to the east. The chargeability anomaly over the Mo mineralisation appears to be reflecting a combination of disseminated pyrite and molybdenite observed in the historic drilling (Figure 3).
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This article includes content from Augustus Minerals, 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.
AUG:AU
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.
