Great Pacific Gold Provides Drilling Update at Hampore Target at Kesar and Commences Project-Wide Airborne Magnetics Survey

In This Article:

Vancouver, British Columbia--(Newsfile Corp. - February 6, 2025) - Great Pacific Gold Corp. (TSXV: GPAC) (OTCQX: FSXLF) (FSE: V3H) ("Great Pacific Gold," "GPAC," or the "Company")  is pleased to announce that drilling has commenced at the high-priority Hampore target within the Kesar Project ("Kesar" or the "Project") in Papua New Guinea ("PNG"). Additionally, the Company has commenced a Mobile Magnetotelluric (MobileMT) geophysical survey across the broader project area to refine geological targets for future exploration and drilling.

Key Highlights:

  • Initial drilling at Hampore, which has commenced, is designed to test beneath a recently identified high-grade existing outcrop identified through mapping and rock chip sampling, which returned exceptional gold values, including: 110 g/t gold (KCRX24120) and 93.3 g/t gold (KCRX24119) - see release dated December 12, 2024.

  • High-resolution airborne Mobile MT geophysical survey underway to inform further drilling with approximately 450 line-kilometers flown to-date (52% complete)

  • Construction of multiple diamond drill pads is underway to test a variety of high-priority targets identified through geological mapping and high-grade rock chip sampling across Hampore.

"Drilling is well underway at Hampore, which has demonstrated exceptional grades and extensive sulphide mineralization in surface samples to-date," stated Greg McCunn, CEO of Great Pacific Gold "We are quickly testing our theory that Hampore and Fufunambi in the East Vein Zone represent the core feeder zone of the extensive system that makes up Kesar. The Mobile MT survey and the key observations made recently by our team and consultants will be invaluable in gaining a more fulsome understanding of this tremendous Project."

Geological Insights from Hampore

Preliminary geological interpretations by Great Pacific Gold geologists aided by Dr. Gregg Morrison, a consultant to GPAC, on the East Vein System at Hampore (Figure 1) shows:

  • The East Vein appears to be a part of an epizonal intermediate-sulfidation polymetallic lode system, likely linked to an intermediate intrusion.

  • Gold mineralization from rock chip samples appears to occur in two distinct styles:

    1. Bonanza Free Gold in arsenopyrite-rich quartz veins, often associated with Bi, Te, and Se.

    2. Electrum-Base Metal Veins within sulfide-rich breccias containing galena, sphalerite, and pyrite, enriched in Ag, As, Sb, Pb, and Zn.

  • Strong Vertical Mineralization Potential: The system exhibits well-defined metal zonation, transitioning from an As-Sb-Au zone into Pb-Zn-Ag and Cu-rich domains, indicating the potential for deeper gold-bearing structures.

  • Hydrothermal Breccias as Prime Targets: The best gold grades (up to 110 g/t Au) are found in hydrothermal breccias with fine crystalline quartz and arsenopyrite, suggesting late-stage mineralization overprinting earlier base metal phases.