Fancamp Successfully Completes Spring Drill Program at Stoke Intersecting 98 metres of Disseminated Copper Mineralization

In This Article:

Fancamp Exploration Ltd.
Fancamp Exploration Ltd.

Figure 1

Stoke Regional Map
Stoke Regional Map

Figure 2

Longitudinal Section – Grand Prix and Copper Zones
Longitudinal Section – Grand Prix and Copper Zones

VANCOUVER, British Columbia, Sept. 08, 2022 (GLOBE NEWSWIRE) -- Fancamp Exploration Ltd. (“Fancamp” or the “Corporation”) (TSX Venture Exchange: FNC) is pleased to announce the completion of its spring drilling program at the Stoke Project, situated in the Eastern Townships of Quebec (Figure 1). Notably, this work, representative of over 1,100 metres of drilling, led to the intersection of the widest sulphide mineralization discovered at the project to date, validating the potential the Stoke-Weedon belt provides for the discovery of copper-rich VMS type deposits (refer to press release dated March 22, 2022).

Fancamp has drilled a total of 1,119 metres in 3 holes during June, over the Grand Prix and Copper Zone of the Stoke property. This program aimed to evaluate the down-dip and down-plunge extension of hole ST-2013-06, which had intersected 6.4 metres @ 7.29% Cu and 17.6 g/t Ag (refer to Hole ST-2011-06, MRN Report GM 66485, 2012) and has now defined mineralization to a vertical depth of approximately 250 metres.

Highlights

  • Hole STDD-22-05 intersected 98.0 metres @ 0.12% Cu (from 275 to 373 metres – downhole length) (Table 1, Figure 2).

  • Hole STDD-22-06 intersected 98 meters of disseminated to semi massive pyrite with specs and stringer of chalcopyrite within a broader zone of 110 metres of intense black chlorite and sericite alteration. Within that interval, several zones exhibiting up to 20% pyrite with trace to 2-3% chalcopyrite were noted.

“Fancamp’s 2022 drilling programs have been providing positive and sustainable results which substantiate management’s exploration plans and corporate strategy, especially on the back of Fancamp’s recently announced strategic sale of the Company’s interests in its Koper Lake mining claims (as reported in press releases dated July 21, 2022, August 10, 2022, September 1, 2022, and September 2, 2022). Today’s announcement of our latest exploration results continues to highlight the prospective extension and proof of mineralization potential of our Stoke Project, building on known historical exploration indicators to new exploration targets and areas of interest. The continuous investment in geological study and exploration by the Company continues to deliver high quality results on which to leverage future exploration and growth initiatives.” – Rajesh Sharma, President and Chief Executive Officer of Fancamp.

Figure 1 – Stoke Regional Map is available at: https://www.globenewswire.com/NewsRoom/AttachmentNg/b48a293c-4185-43fa-b40a-2b69241d0915

Table 1: Stoke Project Drill Results

Hole ID

Prospect

East

North

From

To

Width

Grade

 

 

 

 

 

 

UTM

UTM

(m)

(m)

(m)

Cu (%)

Zn (%)

Pb (%)

Ag (g/t)

Au (g/t)

STDD-22-04

Stoke

285227

5044781

190

192

3

0.24

0.1

0.25

1.3

0.03

STDD-22-05

Stoke

285639

5044860

19

20

1

0

0.01

0.01

<0.2

1.41

 

 

 

 

275

373

98

0.12

0.02

0

0.4

0.01

 

 

 

 

Including

 

 

 

 

 

 

 

 

 

 

 

297

298

1

1.12

0.01

0

2.6

0.01

 

 

 

 

317.25

322

4.75

0.27

0.05

0.01

1.5

0.02

 

 

 

 

348

353

5

0.28

0.01

0

0.8

0.01

 

 

 

 

And

 

 

 

 

 

 

 

 

 

 

 

401.35

402.35

1

0.6

0.01

0.01

2.4

0.03

STDD-22-06

Stoke

284166

5044426

No significant assay results

 

 

 

 

 

 

Outlook

Fancamp and Mira Geoscience Ltd. previously completed the construction of a 3D model for the Stoke project which indicated the property geology is comprised of a main stratigraphic sequence consisting of a volcano-sedimentary succession of bi-modal volcanic units overlain by sedimentary packages. A breakthrough from the 3D modelling interpretation was the development of paleo reconstruction of the stratigraphical units which led to the discovery of a series of either potential synvolcanic faults and/or graben type depression at the paleo surface defined by the exhalative horizon situated at the mafic–felsic contact. These depressions are often the focus of metals deposition and synvolcanic growth faults are often the first-order control on the flow of metal-bearing hydrothermal fluids. Supported by this analysis, the spring drill program at Stoke aimed to test the paleosurface to uncover potential metal concentrations and to test the exhalative horizon associated with interpreted syn volcanic growth faults.