Unlock stock picks and a broker-level newsfeed that powers Wall Street.
Bell Copper Provides Corporate Update

In This Article:

Vancouver, British Columbia--(Newsfile Corp. - December 11, 2024) - Bell Copper Corporation (TSXV: BCU) (OTCQB: BCUFF) ("Bell Copper" or the "Company reports an update on the three year research program being performed by the Arizona Geological Survey ("AZGS"), in collaboration with the University of Arizona Department of Geosciences ("UA"). These entities, funded by the United States Geological Survey and the State of Arizona, are assessing the potential resources of critical minerals in Arizona, including the Company's 100% owned Big Sandy porphyry copper project, a large, concealed porphyry copper-molybdenum project located in northwestern Arizona, approximately 30 kilometers from the Company's Perseverance Project.

Big Sandy Research

Ongoing research of Bell Copper's Big Sandy BS-3 drill core led by Dr. Carson Richardson of AZGS and by Dr. Hervé Rezeau of UA, is ultimately directed toward evaluating Big Sandy's role (alongside porphyry copper occurrences across Arizona) in addressing the US's supply of critical elements, notably copper, molybdenum, rhenium, and antimony. Exports of antimony by China, the world's largest supplier, were halted in an outright ban last week, highlighting the need to identify secure domestic supplies of this element, used primarily in munitions and specialty adhesives.

Results of AZGS's and UA's independent age dating of zircon from porphyry in Bell Copper's BS-3 porphyry intersection and zircon from the Diamond Joe porphyry root were presented in September at the annual meeting of the Geological Society of America (Chappell et al., 2024). This research concluded that "the geochronology of the igneous phases in the two locales overlaps within error" which "supports the hypothesis that Big Sandy is the offset upper portion of the Diamond Joe porphyry system."

AZGS's and UA's analysis of the BS-3 drill core by reflected light microscopy (photos below) shows that primary copper mineralization "mainly consists of quartz-sulfide-sulfosalt veinlets associated with pervasive sericitization of the porphyry host rock. Petrographic analysis shows that subsequent chalcopyrite and bornite as well as galena, sphalerite, and tennantite-tetrahedrite (fahlore) (Figs. B, C) postdate the deposition of pyrite hosting chalcopyrite and bornite inclusions (Fig. A). More localized Cu-rich sulfides include digenite, bornite, and covellite, which crosscut, brecciate, and fill fractures within the earlier mineral assemblages (Figs. D, E). Quartz-pyrite-molybdenite-chalcopyrite and quartz-pyrite-molybdenite veinlets along with some of these veinlets crosscut the Cu-rich sulfide-pyrite mineralization, indicating multiple episodes of pyrite and molybdenite precipitation."