PJX Resources' Drilling Identifies Venting Type Environment That Supports Sullivan Style Sedex Mineralisation

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TORONTO, ON / ACCESSWIRE / September 5, 2024 / PJX Resources Inc. ("PJX" or the "Company") is pleased to announce that on-going drilling at the Dewdney Trail Property has encountered geology that supports the potential to discover a Sedimentary Exhalative (Sedex) type deposit. Of the 3 holes drilled to date the deepest into the mountain has intersected a 20m (estimated true width) fragmental with abundant to semi-massive sulphide mineralisation at 275m. The mineralisation appears to be predominantly iron sulphide (pyrrhotite and pyrite) with visible trace amounts of copper sulphide (chalcopyrite) and zinc sulphide (sphalerite) (see photo A). This style of mineralisation supports a venting environment, which is what occurs at the Sullivan Sedex deposit located approximately 20 km west of the Dewdney Trail Property in Southeastern British Columbia, Canada.

Photo A - Fragmental unit with iron sulphide (pyrrhotite and pyrite) in the matrix and what appear to be iron sulphide clasts in places. Zinc sulphide (sphalerite) and copper sulphide (chalcopyrite) are locally visible in trace amounts (samples have been sent for analysis).

The source of the Sullivan style and grade zinc, lead, and silver mineralisation discovered late last year at surface in boulders in talus material at the base of a mountain slope has not yet been identified by drilling (see photo B). In addition, the zinc and lead mineralisation in outcrop discovered late last year appears to occur in large blocks and/or fragments of stratigraphy that may have collapsed into a sinking basin which can happen in Sedex environments. Additional drilling is required on strike to the north and south as well as higher on the mountain which is stratigraphically above the fragmental unit. Drilling is also required at depth, stratigraphically below the fragmental unit, because of what appear to be massive iron sulphide clasts in part of the fragmental unit (see photo C).

Photo B - Sample STM-23-1 (6.71% zinc, 2.23% lead, 16.05 g/t silver, 1258.9 ppm or 0.12% copper) Strongly magnetic boulder found in talus at base of the moutnain slope late last year. Sphalerite (zinc sulphide), galena (lead sulphide), and iron sulphides (pyrite, pyrrhotite) occur banded or bedded in appearance as seen above. The mineralisation also occurs in the groundmass of the rock.

Photo C - Apparent Iron Sulphide (pyrrhotite and pyrite) clasts in fragmental.

John Keating, President of PJX, commented, "We are very pleased with the results from these initial drill holes. What we've encountered in the fragmental appears to be predominantly iron sulphides. However, having visible trace concentrations of zinc and copper sulphide minerals supports a mineralizing system with potential to produce higher concentrations of copper, zinc, and/or lead horizontally along strike as well as vertically in multiple sedimentary horizons. This type of transition in mineralisation occurs in Sedex environments. So far, we have only tested part of the northern edge of the large magnetic anomaly. We are working with New Age Drilling Solutions to bring additional drills to the property and expand testing. The well mineralized boulders with zinc, lead, and silver discovered late last year also support the potential for more significant zinc, lead and/or copper content. Results of our work along with maps and sections are expected to be announced when the drilling has been completed and results compiled."