FSX to Acquire Significant Papua New Guinea Mineral Exploration Land Package
Fosterville South Exploration Ltd. (FSX) has announced an agreement to acquire a 2166 sq. km mineral exploration land package in Papua New Guinea from Wild Dog Resources Inc. (WDR). This acquisition includes multiple Exploration Licenses (EL) and Exploration License Applications (ELA). Key highlights of the acquisition feature a contiguous 614 sq. km project adjacent to K92 Mining Inc. exploration tenements, enhancing FSX's existing gold land package in Australia. The land package presents both early and advanced stage exploration targets, with a focus on high-grade epithermal vein and porphyry style mineralization. FSX's strong cash position post-transaction will support advancing these assets, leveraging their team's experience in Southeast Asia. The deal is expected to increase FSX's potential for discovering Tier 1 Copper-Gold deposits in PNG.
- Acquisition of 2166 sq. km mineral package enhances exploration footprint in Papua New Guinea.
- Includes projects contiguous with K92 Mining, indicating strong geological potential.
- FSX's significant cash position will enable continued development and exploration post-acquisition.
- Potential for discovering high-grade epithermal vein and porphyry style mineralization.
- None.
Highlights:
- 2166 sq. km land position assembled via acquisition of a variety of EL and ELAs
- including 614 sq. km project contiguous with and SE of K92 Mining Inc exploration tenements
- including 130 sq. km project contiguous with and NW of K92 Mining Inc. tenements, 10km from mining operations
- PNG EL and ELAs will compliment extensive gold land package of FSX in
Australia
The total PNG land package to be acquired by FSX includes both early stage and advanced stage exploration targets with high grade epithermal vein and porphyry style mineralization present. FSX has a significant cash position and therefore, post-transaction, will be well positioned to advance these projects on the ground following up the substantial amount of fieldwork and development of drill targets already completed by WDR over the past two years. FSX team members have significant experience operating within Southeast Asian island arc epithermal and porphyry mineralization environments, and specifically in PNG.
FSX CEO
WDR has invested significant capital and time acquiring and advancing these assets in PNG and their hard work and strong technical execution both on the ground and corporately has put in place an excellent foundation for success as we move forward."
WDR CEO
Kainantu Regional Geology, PNG
The Kainantu district is located within the New Guinea Thrust Belt, close to its northern contact with the Finisterre Terrane. The contact is marked by the northwest trending Ramu-Markham Fault, a major suture zone that marks the northern margin of the Australian Craton. The New Guinea Thrust Belt records an early Miocene or older ductile, tight folding event that was followed by middle Miocene intrusions. Late Miocene regional scale low-angle thrust faulting followed, associated with the collision of the Finisterre Terrane. The belt is characterised by a number of north-northeast trending fault zones that commonly host major deposits (K92 Mining).
Locally, the Kainantu area is underlain by greenschist to amphibolite facies metamorphic rocks of the Early Miocene Bena Bena Formation, which are unconformably overlain by the Miocene age Omaura Formation consisting of volcano-sedimentary units and limestone lenses. The overlying Yaveufa Formation comprises basaltic and andesitic flows, agglomerates, volcanoclastic sandstone and limestone. The mid-
Known mineralisation in the area consists of gold and copper skarn deposits, porphyry copper deposits, shear-hosted gold deposits, epithermal vein deposits and gold placer deposits.
Over 35 hard rock and 18 gold placer deposits are known within the area. Of significance are the Kathnell shear-hosted auriferous quartz veins; such structurally controlled veins may be more widespread than proposed previously and offer a new exploration target (Downes, 1993).
Initial exploration work by previous operators has identified two potential deposit types at the project:
- Epithermal gold (Sabudia Hill, Onga Hill and Erandora prospects) and
- Copper-gold porphyry prospects (Mt.
Victor, Mt. Aiyonka, Ebitara and P1 prospects).
Within the licence area, the Mt. Victor Prospect (copper-gold porphyry target) covers an area of 800m by 400m and previous drilling suggests that the prospect area is a multiple phase intrusive complex that is copper and gold mineralized. It is a drill ready prospect in which previous channel sampling has identified the following strong gold grades:
- 38m @ 2.64 g/t Au
- 12m @ 5.5 g/t Au
- 18m @ 2.4 g/t Au
- 10m @ 3.7 g/t Au.
These channel samples are in the central part of the Mt Victor prospect southwest of the former Mt Victor gold mine. Previous drilling was carried out in the 1980s, and all drillholes presented were vertical, which may not have been appropriate for the subvertical fault zones present within the prospect.
Hole ID | E* | N* | Depth | From (m) | Length (m) | Au g/t | Cu ppm | Notes |
CRD58 | 385177 | 9291680 | 64.5 | 0 | 64.5 | 0.18 | 106 | granodiorite intruded by diorite |
DDH89-1 | 384650 | 9291308 | 260 | 234 | 5 | 0.85 | NA | visible disseminated copper mineralization |
DDH89-2 | 384965 | 9291825 | 300 | 43 | 10 | 1.10 | NA | under review |
DDH89-3 | 384873 | 9291562 | 300 | 213 | 10 | 1.20 | NA | under review |
MVD07 | 384746 | 9291253 | 52.8 | 0 | 52.8 | 0.10 | 384 | altered pyritic diorite |
MVD08 | 384831 | 9291327 | 30 | 16 | 14 | 0.19 | 373 | argillic altered QFP |
MVD09 | 384853 | 9291333 | 36 | 34 | 2 | 0.29 | NA | epidote altered intrusive |
MVD20 | 384900 | 9291345 | 75 | 0 | 75 | 0.34 | 304 | argillic altered brecciated porphyry |
MVD21 | 384890 | 9291353 | 48 | 0 | 48 | 0.41 | 329 | diorite/QFP brecciated contact |
MVD36 | 385032 | 9291456 | 24 | 22 | 2 | 14.70 | 463 | altered pyritic porphyry |
MVD40 | 384994 | 9291435 | 38 | 0 | 38 | 3.10 | 1400 | silica epidote altered porphyry |
MVD46 | 384932 | 9291388 | 34.5 | 15 | 19.5 | 0.33 | 117 | epidote pyrite altered porphyry |
MVD50 | 385068 | 9291469 | 29 | 16 | 13 | 0.13 | 722 | clay altered granodiorite |
MVD52 | 384962 | 9291475 | 30 | 14 | 16 | 1.01 | 77 | sericite epidote altered porphyry |
MVD62 | 384704 | 9291152 | 75 | 40 | 35 | 0.12 | 287 | kspar epidote altered porphyry |
MVD63 | 384596 | 9291160 | 48 | 0 | 48 | 0.75 | 373 | diorite intruded by pyritic porphyry |
Initial drilling at the
The Wild Dog project occurs within a major NNE trending structure of at least 26km in length which transect apparent volcanic caldera structures and intrusions. During the Mio-Pliocene at least three volcanic centres, known as the Nengmutka, Keravat and Sikut calderas, were localised along this horst and graben zone. This structural corridor is an epithermal and porphyry hydrothermal-magmatic mineralized field.
The Nengmutka Caldera, which hosts the Wild Dog deposit, is characterised by a suite of calc-alkaline andesite breccia and ash flow tuff known as the Nengmutka Volcanics (Lindley, 1988). This formation has been mapped over an area of 600 km2. Tonalite of the Arabam Diorite intrudes the volcanic sequence and appears to be partly coeval with the caldera related volcanism.
The precious metal prospects are associated with epithermal type veining that contain gold-silver-telluride (Au-Ag-Te) mineralisation. Gold and silver occur as native metals and as telluride minerals. Porphyry copper-gold type mineralization also occurs associated with these intrusion centres that usually underly the epithermal systems. The whole of the recognised belt is held within the Wild Dog tenements.
Within the central part of the Wild Dog project, a significant structural corridor called the "Wild Dog – Gunsap Corridor" occurs. The corridor is at least 15 km long and up to 4 km wide and hosts at least three porphyry copper-gold prospects and several epithermal gold deposits and prospects.
The original Wild Dog epithermal gold deposit occurs within the "Wild Dog – Gunsap Corridor" in the central part of the tenements. It was discovered in 1983, with exploration including extensive mapping, trenching, rock sampling & drilling between 1983 and 2005 by various explorers.
Historical work completed by a previous operator returned significant gold assays. Channel sampling at the Kavursuki Prospect yields 4m at 9.41 g/t Au and at the Kargalio Vein 6m at 11.5 g/t Au.
Drilling of the Kavursuki Prospect by previous explorers, located within the
Hole ID | N | E | RL | Depth | Dip | From (m) | Length (m) | Au g/t | Cu ppm | |
90KVD005 | 9490500 | 395008 | 787 | 85.60 | 101.50 | -45.00 | 5.35 | 1.25 | 12.80 | 1200 |
90KVD009 | 9490834 | 395227 | 758 | 93.85 | 101.50 | -45.00 | 44.65 | 3.75 | 11.21 | 639 |
10KVD016 | 9490464 | 394971 | 798 | 51.00 | 101.50 | -50.00 | 35.44 | 8.06 | 6.49 | 194 |
10KVD017 | 9490464 | 394970 | 798 | 50.00 | 101.50 | -65.00 | 29.08 | 1.12 | 33.70 | 120 |
11KVD019 | 9490496 | 395039 | 807 | 45.10 | 101.50 | -60.00 | 11.10 | 5.25 | 9.45 | 167 |
11KVD020 | 9490537 | 395045 | 805 | 50.90 | 101.50 | -50.00 | 32.45 | 11.05 | 3.18 | 377 |
11KVD025 | 9490809 | 395241 | 752 | 45.20 | 101.50 | -50.00 | 14.75 | 8.15 | 18.77 | 2801 |
11KVD026 | 9490810 | 395272 | 776 | 51.70 | 281.50 | -60.00 | 33.80 | 5.10 | 14.70 | 101 |
11KVD027 | 9490870 | 395252 | 767 | 56.10 | 101.50 | -50.00 | 30.70 | 1.90 | 10.35 | 46 |
Apart from the drilling conducted at the former Wild Dog gold mine there remain several drill intercepts that require further exploration outside of the mine environment as tabulated below, apart from the various trenching and channel sampling targets.
Hole ID | N | E | RL | Depth | Dip | From | Length | Au g/t | Cu ppm | |
86WDD020 | 9489141 | 394278 | 983 | 259.35 | 103.50 | -60.00 | 129.35 | 7.70 | 5.28 | 902 |
87WDD024 | 9489117 | 394316 | 965 | 152.55 | 98.50 | -60.00 | 138.25 | 5.10 | 8.32 | 8556 |
87WDD027 | 9489115 | 394325 | 965 | 200.40 | 98.50 | -60.00 | 117.95 | 6.20 | 19.13 | 786 |
87WDD040A | 9489219 | 394320 | 994 | 280.99 | 103.50 | -60.00 | 148.60 | 4.20 | 12.50 | 4066 |
87WDD045 | 9489235 | 394287 | 988 | 300.20 | 103.50 | -60.00 | 201.30 | 2.85 | 16.94 | 32123 |
87WDD051 | 9489249 | 394257 | 985 | 309.10 | 103.50 | -60.00 | 253.95 | 6.05 | 7.29 | 2054 |
87WDD058 | 9489285 | 394359 | 977 | 285.90 | 101.50 | -60.00 | 147.00 | 12.45 | 4.96 | 6694 |
87WDD064 | 9489179 | 394289 | 1001 | 290.60 | 101.50 | -60.00 | 158.00 | 14.95 | 2.73 | 650 |
87WDD065 | 9489160 | 394330 | 996 | 250.10 | 101.50 | -60.00 | 142.70 | 4.65 | 5.49 | 3246 |
87WDD069 | 9489139 | 394375 | 991 | 123.50 | 101.50 | -60.00 | 88.55 | 7.75 | 7.12 | 7151 |
08WDD111 | 9489393 | 394513 | 906 | 100.00 | 281.50 | -60.00 | 48.40 | 7.10 | 5.47 | 931 |
85WDD014 | 9488708 | 394260 | 954 | 86.20 | 113.50 | -51.00 | 48.25 | 5.25 | 9.79 | 10863 |
86WDP010 | 9488839 | 394302 | 909 | 60.00 | 83.50 | -60.00 | 34.00 | 6.00 | 6.71 | 5047 |
87WDD040A | 9489219 | 394320 | 994 | 280.99 | 103.50 | -60.00 | 164.55 | 13.50 | 8.56 | 3056 |
90WDD086 | 9488948 | 394337 | 890 | 79.00 | 78.50 | -50.00 | 18.45 | 11.25 | 16.22 | 3473 |
97WD098 | 9489389 | 394487 | 905 | 39.00 | 98.50 | -45.00 | 12.00 | 8.00 | 9.73 | NA* |
NA* - not assayed or not available.
Hole ID | North | East | RL | Depth | Dip | From | Length | Au g/t | Cu ppm | |
MRC01 | 9487963 | 393871 | 968 | 20.00 | 0.00 | -90.00 | 2.00 | 18.00 | 3.05 | 3084 |
MRC02 | 9487978 | 393874 | 971 | 30.00 | 0.00 | -90.00 | 0.00 | 18.00 | 3.07 | 1053 |
90WDD087 | 9488091 | 394082 | 1021 | 61.95 | 101.50 | -50.00 | 7.30 | 1.35 | 5.02 | 1650 |
90WDD088 | 9488104 | 394070 | 1023 | 40.30 | 101.50 | -50.00 | 21.30 | 1.55 | 3.95 | 25 |
MMD003 | 9486870 | 393532 | 924 | 104.00 | 133.00 | -50.00 | 2.35 | 4.42 | NA* | |
MMD006 | 9486770 | 393479 | 945 | 122.05 | 133.00 | -50.00 | 2.55 | 4.16 | NA* |
Additionally, multiple samples collected from a historic stockpile near the
The exploration program at Wild Dog will initially focus on drilling the copper-gold Magiabe porphyry target as well as testing the potential existence of an arrowhead intrusion complex at depth beneath the Wild Dog zone (Figure 5).
Exploration at Kesar Creek has identified the presence of semi-massive copper sulphides associated in quartz veins paralleling the Kora gold deposit as well as the potential for a copper-gold porphyry deposit. Although limited exploration has been carried out at Kesar Creek, initial rock sampling programs returned high-grade gold-copper-silver values including:
- Rock sample no 14128 at 11.5 g/t Au
- Rock sample no A1428 at 11.9 g/t Au
- Rock sample no 9231F at 10.6 g/t Au
- Rock sample no 14236 at 11.6 g/t Au, 29 g/t Ag, 360 ppm Cu
- Rock sample no. A14023 at 30.4 g/t Au, 240 g/t Ag, 1300 ppm Cu
Terms of Transaction
Via the execution of a non-binding term sheet, Fosterville South and WDR have agreed to negotiate and settle the terms of a definitive share purchase agreement whereby Fosterville South will acquire all the issued and outstanding securities of WDR. Management of both WDR and FSX support this transaction. In consideration of WDR, Fosterville South will issue a total of 16.8 million common shares to the shareholders of WDR, 526,835 share purchase warrants to the warrant holders of WDR and grant 1,553,520 options to the stock option holders of WDR. The transaction is subject to
FSX began with two,
All of FSX's properties, with the possible exception of Moormbool, have had historical gold production from hard rock sources despite limited modern exploration and drilling. Victorian exploration is continuing to focus on specific key targets where results to date indicate excellent exploration potential.
The technical content of this news release has been reviewed, verified and approved by WDR Director,
On behalf of the Company
Chief Operating Officer and Director
Information set forth in this news release contains forward-looking statements that are based on assumptions as of the date of this news release. These statements reflect management's current estimates, beliefs, intentions and expectations. They are not guarantees of future performance. Fosterville South cautions that all forward looking statements are inherently uncertain and that actual performance may be affected by many material factors, many of which are beyond their respective control. Such factors include, among other things: risks and uncertainties relating to Fosterville South's limited operating history, its exploration and development activities on the Lauriston, Golden Mountain, Providence and
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