Overview

Thunderstruck's 100% owned, high-grade Nakoro zinc/copper volcanic massive sulphide (VMS) prospect boasts a historical resource of 4.3% CuEq and sits within an 8 km untested prospective geologic horizon which is open at depth and along strike.   Nakoro is hosted within the same geologic unit as Thunderstruck’s highly prospective Korokayiu VMS prospect.

Location

The Nakoro VMS prospect is located on Fiji’s largest island, Viti Levu.   Nakoro is 25km north and contiguous to Thunderstruck’s Korokayiu VMS asset, allowing for the possibility of a hub and spoke mining district with central processing plant.  The prospect sits within the 148km2 land package of Special Prospecting License No. 1425 and is approximately 50 km northwest of the capital and deep-water port of Suva.

History

Nakoro’s zinc/copper potential was initially discovered through country-wide stream sediment sampling programs undertaken by Barringer in the 1960’s.  Barringer entered a joint venture with Australian Anglo American who carried out two drill campaigns in 1975 and 1977 totaling 1850m with 20 drill holes having an average depth of 130m.  Anomalous intercepts¹ include: 

• 12 m of 12.7 % Zn, 0.3% Cu (NKD-2)
• 7.4 m of 7.2 % Zn, 0.30% Cu (NKD-12)
• 23.2 m of 5.1 % Zn, 0.05% Cu (NKD-13)
• 4.44m of 8.8% Zn, 0.37% Cu (NKD-15)

¹Drill intercepts are considered historic and are not NI 43-101 compliant.

Shallow vertical “backpack” diamond drilling discovered a near-surface Cu-Zn rich zone with several anomalous drill intersections including:​

• 1.6m @ 2.9% Cu, 1.3% Zn and 33.0 g/t Ag (NKD-111)​
• 3.0m @ 2.6% Cu, 6.6% Zn and 26.0g/t Ag (NDK-123)​
• 0.8m @ 1.98 % Cu, 3.06 % Zn, and 131 g/t Ag (NKD-135)​

More recently, Thunderstruck revived exploration at Nakoro with geochemical and geophysical programs aimed at expanding known mineralization.   Systematic mapping and sampling increased surface expressions of massive sulphides and gossans by 2km along strike, and new drill targets were delineated from results of Thunderstruck’s Induced Polarization (IP) geophysical program in 2023.

Geology and Mineralization

Nakoro is located in hilly grassland with distinct brecciated and massive zinc and copper mineralization. 

Geologically, Viti Levu has been exposed to a complexity of crustal plate rotations and has been dominated by island arc development followed by rifting, like that of neighboring Pacific Rim countries. Magmatism, precious, and base metal emplacement occurred episodically throughout the evolution of the Fijian platform. The oldest known mineral occurrences are hosted within low-K tholeiitic volcanics of the Wainimala Group, host to the Nakoro and Korokayiu VMS prospects.  The Wainimala Group are of Late Oligicene to Middle Miocene Age (28-16 million years) consisting mainly of basaltic volcanic and, to a lesser extent, sedimentary rocks which were subjected to extensive faulting and folding.

Figure 1:  Map of Viti Levu, Fiji.  Nakoro is hosted in the Wainimala Group. (Black dashed line is the trace of the Wainimala Oriclinal Flexure) 

The Nakoro prospect area contains numerous limonitic gossans over a strike length of 700m (Figure 3).  Beneath the gossans is intense silicification and phyllic, argillic alteration, with the silification being the more extensive.   Mineralization occurs as massive sulphides, sulphide rich veinlets and within silicified rocks as sulphide disseminations (Figure 2).  Common minerals include pyrite, sphalerite, barite, chalcopyrite, bornite and covellite with minor galena and tetrahedrite-tennanite.

Figure 2: Nakoro gossans with massive sulphides

Historic drilling intersected a massive sulphide zone to a depth of approximately 125 m and has shown the zone to strike northeast (similar strike to the gossans), with a shallow dip to the southeast (Figure 3).  Mineralization is open in all directions.

Figure 3: Nakoro prospect geology

Exploration Potential

The Nakoro VMS prospect sits on an 8km prospective geologic horizon with high-grade historical drill intercepts of copper and zinc and favourable topography, weather conditions and a supportive local community.   Recent mapping and sampling programs extended the known mineralized VMS system from 700m to 2.7km, while geophysics provided target definitions for further drilling.  The targets highlighted at Nakoro warrant further exploration through modernized, higher resolution techniques and drilling of high-grade zones to expand the known extent of mineralization.

Overview

Thunderstruck's 100% owned Nakoro VMS (volcanic massive sulphide) prospect is located in Fiji with anomalous copper and zinc intercepts from historical drilling with recently discovered surface expressions, and mineralization that is open at depth and along strike. The prospect sits within an 8 km untested prospective geologic horizon highlighted through the interpretation of regional magnetics. Nakoro is hosted within the same geologic units as Thunderstruck’s highly prospective Korokayiu VMS prospect.

Location

The Nakoro VMS prospect is located on the southern part of Fiji’s largest island, Viti Levu, and is approximately 50 km east south east of Nadi. The prospect sits within Special Prospecting License No. 1425 and, along with landowner agreements, has been renewed for 5 years, the maximum allowed under Fijian exploration policy. The Nakoro prospect is part of a 148 km2 property, located 50 km south of the Vatukoula gold mine, which has produced 7 million ounces of gold .

History

The Nakoro VMS prospect was initially highlighted by country wide stream sediment sampling programmes undertaken by Barringer Fiji Ltd. (Barringer) In the 1960’s. Barringer entered a joint venture with Australian Anglo American Ltd. (Anglo) in 1974 who carried out two drill campaigns in 1975 and 1977. High grade zinc intercepts from Anglo include 12 m of 12.7 % zinc, 7.4 m of 7.2 % zinc and 23.2 m of 5.1 % zinc1. After laying untouched for years VMS exploration was revived on the property in 2006 with surface sampling aimed at discovering surface expressions of high-grade historic drill intersections. Recent work includes anomalous near surface shallow “back pack” drill intercepts of zinc, copper and gold.

Geology and Mineralization

Geologically, Viti Levu has been exposed to a complexity of crustal plate rotations and has been dominated by island arc development followed by rifting, like that of neighboring Pacific Rim countries. Magmatism, precious, and base metal emplacement occurred episodically thought out the evolution of the Fijian platform. The oldest know mineral occurrences were emplaced within low-k tholeiitic volcanics of the Wainimala Group, host to the Nakoro and Korokayiu VMS prospects, both proximal to the major intrusive Colo Plutonic Suite.

The Nakoro prospect area contains numerous limonitic gossans over a strike length of 700 m. Below the gossans is intense silicification along with phyllic and argillic alteration, as suggested Anglos drilling. Historic drilling has shown the zone to strike north east, like gossans, with an interpreted dip angle of 10o to the south east. Mineralization occurs as massive sulphides, sulphide rich veinlets and within silificied rocks as sulphide disseminations. Common minerals include pyrite, sphalerite, barite, chalcopyrite, bornite and covellite with minor galena and tetrahedrite-tennanite. Historic drilling intersected a massive sulphide zone to a depth of approximately 125 m, with an average width of 7m, over a strike length of some 300m. Mineralization is open in all directions.

Exploration Potential

The exploration potential for VMS deposits is being demonstrated through current exploration work on Thunderstrucks Korokayiu deposit. The Nakoro VMS prospect, like Korokayiu, is hosted within the Wainamala Group, has historical high-grade intercepts of copper and zinc, and recent work detailing near surface anomalous copper and zinc values. The targets highlighted at Nakoro warrant further exploration through modernized, higher resolution techniques and drilling of high grade zones to expand the known extent of mineralization.

¹Drill intercepts are considered historic and are not Ni 43-101 compliant nor have they been verified.

The Nakoro prospect is a zinc-copper volcanogenic massive sulphide prospect located in the northern portion of SPL 1425. A diamond drilling program carried out by Anglo American in the 1970’s intersected anomalous values including:-

• 12 metres @ 12.7% zinc, 0.3% copper and 56g/t silver,
• 23.2 metres @ 5.1% zinc, 0.5% copper and 22g/t silver,
• 7.4 metres @ 7.2% zinc, 0.3% copper and 54g/t silver.

Recent shallow diamond drilling has located a new copper-zinc rich zone close to the surface with several anomalous drill intersections including 1.3 metres @ 3.3% copper, 1.5% zinc, 37.6 g/t silver and 1.6 metres @ 3.0% copper, 10.9% zinc and 40.5 g/t silver. In another area a float sample assayed 21.1% copper. This suggests there may be zones   with higher copper values in the prospect area increasing the chance of finding an economic deposit.

Geophysical interpretative work carried out in 2012 indicated that the prospective horizon extends over 8 kms.

Selective surface grab samples of zinc rich nodules,

(sphalerite-rich) assayed 2.6% copper, 27.5% zinc and 177 g/t silver.