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Nimy Resources: Drilling returns copper-silver-zinc intersection followed by 487m nickel-copper ultramafic zone - Mons Nickel Project, WA


-          Excellent result from first hole at the Dease prospect provides strong evidence that Mons hosts additional mineralised styles.

 

-          The first diamond drill hole at the Dease prospect within the Mons project (NRDD004) has successfully intersected the first of three targeted MLEM conductive anomalies.

 

-          The drill hole was designed to target a conductive anomaly modelled to be between 325-375m downhole. The anomaly was intersected where it was anticipated.

 

-          Logging has recorded porphyritic felsic and mafic rocks from 216m to 291.2m passing into a intercalated schistose mafic and porphyritic felsic (porphyry) rocks zone to 383.6m, thereafter ultramafic rock was drilled to 870.8m end of hole.

 

-          The conductive anomaly returned elevated copper, silver, zinc and sulphur values within visible sulphides when tested with a portable XRF.

 

-          The 487.2m ultramafic interval confirmed to carry nickel and copper mineralisation when tested with portable XRF.

 

-          Down-hole, electro-magnetic survey scheduled for mid-July. 

 

Nimy Executive Director, Luke Hampson, commented:

 

The successful intersection of the first conductor plate drilled at Dease opens up the potential for additional mineralisation styles at the Mons Project.

 

Result follows intersection of nickel and copper in the first holes at nearby Godley target and we have now intersected anomalous nickel and copper over significant widths at both Dease and Godley.

 

Drilling has been completed at the Dease Gossan and currently in the logging and sample preparation process and we look forward to these results adding further information to the Dease prospect profile”.

 

Summary

 

Nimy Resources (ASX:NIM) is pleased to announce the first diamond drill hole at the Dease prospect within the Mons project (NRRD004) has successfully intersected the first of three interpreted anomalous Moving Loop Electromagnetic (MLEM) conductors.

 

The drill hole was collared (MGA collar coordinates 661440E, 6678494N, dip 60⁰ and azimuth 305⁰) targeting the conductive anomaly estimated to be intersected between 325 – 375m downhole.

 

The hole has been logged from 216m and encountered porphyritic felsic and mafic rock from 216m to 273.1m passing into an intercalated schistose mafic and felsic porphyry zone to 383.6m whereby ultramafic rock (minor mafic and felsic) was drilled to 870.8m (end of hole).

 

The conductive anomaly sits within this schistose mafic-porphyry zone which returned elevated copper, silver, zinc and sulphur values associated with visible sulphides when tested with a portable pXRF.

 

Below the intersection of the conductive anomaly (Figure 2) the komatiitic ultramafic began at 383.6 continuing to the end of hole at 870.8 (487.2m).   

 

The 487.2m ultramafic interval returned anomalous nickel and copper readings when tested using a portable XRF.

 

Coupled with the first diamond drilling (two holes) at Godley, the Dease hole confirms that both prospect  areas contain  extensive and thick ultramafic units hosting nickel and copper mineralisation. Downhole electro - magnetic survey’s will commence in mid - July at completed holes (Dease and Godley).

 

The primary objectives of obtaining lithological, structural, and mineralisation information have been met on the first two holes at Godley whilst the Dease hole remains open at depth.

 

The significance of the copper, silver, and zinc mineralisation within the conductive plate and its relationship, if any, with a copper-zinc-lead-gold in soil geochemical anomaly approximately 2.5 km south west of the conductive plate is being assessed. 

 

Drill hole NRDD004 has intercepted the middle plate approximately 2.5 km northeast of the coincident soil anomalies.  Reverse circulation drill hole NRRC006 drilled in October 2020 (178m EOH) above the plate anomaly, reported anomalous intervals of nickel, copper and gold.

 

 

Figure 1 - Conductive plates plan – NRDD004 (centre plate) drilled first

 

 

Figure 2 – Diamond Hole – NRDD004 – Cross section

 

Summary of significant intersections in NRRC006

 

Table 1 and Figure 3 below detail significant intersections in RC hole NRRC006 based on geochemical assays.  A cut-off grade of 1500 ppm Ni (0.15%) has been applied to reflect the presence of anomalous mineralisation and in consideration of the stage of exploration. Details of the RC drilling and sampling techniques are provided in the Table 1 declaration. The location of the Dease target relative collars are given in Table 3.

 

 

Table 1 – Hole NRRC006 – significant intersections (Ni>1500ppm, Cu>300ppm, Au>20ppb)

 

 

Figure 3 - Reverse Circulation Hole NRRC006 assay values downhole

 

The interval in hole NRRC006 encountered ultramafic rock at 57m until the end of hole at 178m with four quartz vein intersections within the ultramafic (max intercept 2m) MgO levels averaged 24.23% from 57m - 178m (end of hole) with a peak MgO value of 31.67%. Anomalous copper (>300ppm) was restricted to clay and saprolite, however, a quartz vein in fresh rock intercepted 1270ppm (0.13%) from 114-115m. Gold was primarily located in the sap-rock with an anomalous 3m interval (70ppb including 1 metre at 142ppb) within 42-45m,, additionally a 37ppb Au quartz vein intercept was returned from 159-160m. Details of the NRRC006 intersections are provided in Table 1 and Figure 3.

 

Nimy Resources – Copper Anomaly (previously reported)

 

Reference 18/11/21 - Nimy Resources Prospectus and Independent Technical Assessment Report

 

COPPER MINERALISATION

 

The centre of tenement E77/2255 contains anomalous surface samples indicative of copper (984 ppm Cu) and gold (92 ppb Au). Mineralisation coincident with potassium zone alteration visible on radiometric imaging auger sampling over the area has defined anomalous Au, Cu, Zn and Pb (Figure 4). Regional and ground magnetics indicate two magnetic highs and a magnetic low proximal to the potassium alteration zone. Based on modelling of the surface geochemical signatures, an initial concept indicates a potential copper porphyry system. Further work is underway to define the relationship among the varying critical rock types.

 

 

Figure 4Auger sampling over the area has defined anomalous Au, Cu, Zn and Pb,

 

( indicates position of NRDD004)

 

Figure 5, Figure 6 and Figure 7 all depict mineralisation within the MLEM target zone in hole NRDD004

 

 

 

Figure 5Copper, Silver and Zinc mineralisation in sulphide at 340.75m

 

 

Figure 6Diamond Hole -NRDD004 – Copper, Silver and Zinc mineralisation in sulphide at 342.9m

 

 

Figure 7 – Diamond Hole - NRDD004 - Copper, Silver and Zinc mineralisation at 367.4m

 

Figures 8 to 11 depict nickel and copper sulphide mineralisation within the thick komatiite underlying the interpreted conductive plate.

 

 

Figure 8 - Diamond Hole - NRDD004 Nickel and Copper mineralisation 436.85 – 440.3m

 

 

Figure 9 - Diamond Hole - NRDD004 - Nickel and Copper mineralisation at 441.4m

 

 

Figure 10 - Diamond Hole - NRDD004 - Nickel and Copper in sulphide at 508.0m

 

 

Figure 11 - Diamond Hole - NRDD004 Nickel and Copper in sulphide at 544.0m

 

Dease prospect drill collars

 

Hole Identifier

MGA collar coordinates*

EOH depth (m.)

Hole Orientation

Easting

Northing

Elevation

Dip

Bearing

NRRC006

661,585

6,679,116

425

178

-90°

000°

NRDD004

661,440

6,678,494

425

870.8

-60°

305°

Table 2 Dease drill hole information

 

 

Work Management Process

 

Core logging, photography, specific gravity, structural, magnetic suseptability and sample preparation have been completed in Kalgoorlie by an independent consultant prior to transport to Perth for geochemical analysis.

 

Nimy collated pXRF readings of Ni, Cu, Ag, S, MgO and SiO2 levels to assist in lithological logging and initial identification of mineralisation styles present.

 

An Olympus Vanta Series pXRF was used to collect the readings.

 

Work plan status

 

The Company’s immediate work plan includes the following:

 

-          Hole NRDD006 (Gossan area – Dease prospect, Figure 12) drilling completed – pXRF to be completed - core to be packed and despatched to Kalgoorlie

 

-          Hole NRDD003 (conductor plate – PHDD001) drilling commenced

 

-          Awaiting assay results on first two diamond holes - NRDD001, NRDD002

 

-          Additional geochemical and petrography test-work is to be completed on selected sections of the core to determine the mineralogy and mineralisation types in each of the discrete anomalous zones with higher nickel and copper grades.

 

-          Drill holes are to be reviewed to determine the stratigraphic orientation of the ultramafic komatiite flow or flows, lithological connections of the mineralised zones and the structural orientation of the basal contact.

 

-          Downhole EM (DEM) will be completed on Dease / Godley prospect area (commencing mid-July)

 

-          Current and historic information will be combined and used to plan additional exploration at both the Dease and Godley prospects.

 

-          Nimy continues to update Mons exploration potential thus providing a pipeline of exploration targets

 

 

Figure 12 - Mons Nickel Project – Zone A Exploration Zones including the Dease prospect

 

Previous Related Announcements

 

18/11/21  Nimy Resources Prospectus and Independent Technical Assessment Report

8/02/22 Three conductive EM plates identified at Mons Nickel Project

17/03/22 Godley diamond drilling update

29/03/2022 Gossan discovered at Dease up to 0.96% Nickel

13/04/2022 Semi - Massive Sulphide intercepted at Godley

 

This announcement has been approved for release by the Board

 

Company Information

Nimy Resources Limited

Christian Price

Executive Director

[email protected]

(08) 9261 4600

 

Investor & Media Information

Read Corporate

Paul Armstrong

[email protected]

(08) 9388 1474

 

COMPETENT PERSON’S STATEMENT

 

The information contained in this report that pertain to Exploration Results, is based upon information compiled by Mr Ian Glacken, a full-time employee of Snowden Optiro Limited. Mr Glacken is a Fellow of the Australasian Institute of Mining and Metallurgy and has sufficient experience in the activity which he is undertaking to qualify as a Competent Person as defined in the December 2012 edition of the “Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves” (the JORC Code). Mr Glacken consents to the inclusion in the report of the matters based upon his information in the form and context in which it appears.

 

FORWARD LOOKING STATEMENT

 

This report contains forward looking statements concerning the projects owned by Nimy Resources Limited. Statements concerning mining reserves and resources may also be deemed to be forward looking statements in that they involve estimates based on specific assumptions. Forward-looking statements are not statements of historical fact and actual events and results may differ materially from those described in the forward looking statements as a result of a variety of risks, uncertainties and other factors. Forward looking statements are based on management’s beliefs, opinions and estimates as of the dates the forward looking statements are made and no obligation is assumed to update forward looking statements if these beliefs, opinions and estimates should change or to reflect other future developments.

 

About Nimy Resources and the Mons Nickel Project

 

Nimy Resources is an emerging exploration company, with the vision to responsibly discover and develop an economic nickel-sulphide project in a Tier 1 jurisdiction, Western Australia.

 

Nimy Resources has prioritised the development of the Mons Project, a district scale land holding consisting of 12 tenements, an area over 1,761sqkm along an 80km north/south strike.

 

Mons is located 140km north of Southern Cross and covers the Karroun Hill Nickel district on the northern end of the world-famous Forrestania nickel belt. Mons features a very similar geological setting to the southern end of the Forrestania belt and the Kambalda nickel belts.

 

The project is situated within a large scale fertile “Kambalda-Style” and “Mt Keith-Style” Komatiite sequences within the Archean Murchison Domain of the Youanmi Terrane of the Yilgarn Craton.

 

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