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ESGold Explores Broken Hill-Montauban Analogue: Unveiling a Potential Larger Discovery
Applying Modern Exploration to Unlock Montauban's Hidden VMS Potential Vancouver, British Columbia--(Newsfile Corp. - March 25, 2025) - ESGold Corp. (CSE: ESAU)
About this update from Esgold Corp
[{"type":"text","content":" Applying Modern Exploration to Unlock Montauban's Hidden VMS Potential Vancouver, British Columbia--(Newsfile Corp. - March 25, 2025) - ESGold Corp. (CSE: ESAU) (OTCQB: SEKZF) (FSE: Z7D) (\"ESGold\" or the \"Company\") is pleased to provide an in-depth geological perspective on the striking similarities between its Montauban Project in Quebec, Canada, and Broken Hill, Australia - one of the world's most prolific polymetallic deposits(1). This detailed geological assessment, led by ESGold's Senior Geologist, André Gauthier, suggests that Montauban may share key geological characteristics with the Broken Hill deposit, pointing to an underexplored mineral system. Parallels Between Broken Hill & Montauban The Broken Hill deposit, discovered in 1883, became the world's largest single source of silver, lead, and zinc, generating over $100 billion in historical production. Its distinct boomerang-shaped, structurally complex massive sulfide lenses were hidden from discovery for decades, much like what ESGold now believes could be the case at Montauban. The Broken Hill deposit in New South Wales, Australia, is widely regarded as the prototypical Broken Hill-type (BHT) lead-zinc-silver ore system, a subclass of volcanogenic massive sulfide (VMS) deposits. The deposit features high-grade silver, lead, and zinc mineralization with significant gold occurrences. It formed through a combination of hydrothermal processes, structural deformation, and remobilization of mineralization over geological time.(1) Figure 1: Generalized longitudinal section at Broken Hill deposit Rhodonite as a Key Indicator of a Broken Hill-Type System Recent sampling at Montauban confirmed the presence of rhodonite, a manganese silicate mineral intimately associated with BHT deposits. At Broken Hill, rhodonite is a hallmark of high-grade metamorphic environments closely linked to lead-zinc-silver mineralization. Its presence at Montauban reinforces geological parallels between the two systems and suggests the potential for previously unrecognized mineralized zones.(1) For more details on the rhodonite discovery, read the full news release here: Click Here Mineralogical observations are preliminary, and the interpretations based on them are conceptual. There is no certainty that further exploration or detailed studies will substantiate these preliminary obser...