Callinex Announces Magnetotelluric ("MT") Geophysical Survey Results over the Descendent Copper-Gold-Silver-Zinc Discovery at the Pine Bay Project

In This Article:

Callinex Mines Inc. logo (CNW Group/Callinex Mines Inc.)
Callinex Mines Inc. logo (CNW Group/Callinex Mines Inc.)

Highlights:

  • MT results provide support that Descendent deposit continues at depth;

  • A second very strong resistivity low anomaly starting 350m below surface interpreted to reveal large target areas along VMS horizons that host the Rainbow and Pine Bay VMS deposits;

  • Conductive borehole pulse electromagnetic anomalies further strengthens target areas identified by MT survey; and

  • MT survey data from the Pine Bay and Odin survey lines are being processed and will be released in the very near future.

VANCOUVER, BC, April 15, 2024 /CNW/ - Callinex Mines Inc. (the "Company" or "Callinex") (TSXV: CNX) (OTCQX: CLLXF) is pleased to announce results from the recently completed magnetotelluric ("MT") geophysical survey on the Company's 100% owned Pine Bay Project (the "Project") located in the Flin Flon Mining District of Manitoba (See news release dated January 29, 2024). The 3km MT survey line over the Descendent discovery and near surface historic Cabin deposit has been collected and processed (Pine Bay Project Plan View with Proposed MT Survey Lines). MT is a deep penetrating geophysical tool that is used in mineral exploration to identify systems that produce conductive minerals such as copper, gold and silver and mapping of geologic features.

Max Porterfield, President and CEO, stated, "The MT survey results over the Descendent deposit provide additional support for and strengthen our conviction of the potential of the Company's newest discovery. Additionally, the emergence of a second stronger anomaly that correlates to existing base metals rich VMS horizons indicate the potential for multiple parallel deposits to exist in proximity to Descendent. We are excited to follow up at Descendent and this significant anomaly in the future."

The MT survey completed over the Descendent discovery, the first of three MT lines completed at the Project to be announced, has been very successful on multiple fronts. Resistivity low survey results strongly correlate with the halo of stringer mineralization (alteration package) enveloping the Descendent discovery which consists of copper-gold-zinc-silver bearing Volcanogenic Massive Sulphide ("VMS") mineralization (MT Survey Descendent Line Cross Section). It is also important to note that the resistivity low anomaly associated with the Descendent VMS system remains open at depth, as supported by other geological, geophysical and geochemical data.

Pine Bay Project 2024 MT Survey Results: Descendent Low Resistivity Cross Section (CNW Group/Callinex Mines Inc.)
Pine Bay Project 2024 MT Survey Results: Descendent Low Resistivity Cross Section (CNW Group/Callinex Mines Inc.)

Of additional exploration relevance, a second stronger and even more widespread, resistivity low anomaly starting 350m below surface and extending to the full depth capability of the MT survey is located to the west of the Descendent MT anomaly and is interpreted to represent a deeply buried, 'blind', very large alteration system, equivalent to the 1,100m by 700m Descendent alteration system mapped on surface. This second resistivity low of importance is interpreted to occupy the axial region of a tight isoclinal fold separating the east-facing Pine Bay VMS horizon from the stratigraphically equivalent, west-facing Rainbow VMS horizon. Drill hole PBM-024, the only drill hole to test near this large resistivity low feature at depth and tracking parallel roughly 185m south of the MT survey line, intersected both the Pine Bay and Rainbow VMS horizons as well as a very thick package of intensely altered felsic volcanic rocks occupying almost the entire distance between the two. As shown in the survey data and as would be expected, the Rainbow and Pine Bay VMS horizons occur along the western and eastern edges of the strong MT, alteration zone-related anomaly.