Regency Silver to Present at MK-Equity Investment Conference in Munich
News related to:Regency Silver Corp · 1 min read
Regency Silver Corp., a Canadian mineral exploration company focused on high-grade gold, silver, and copper in Mexico, is set to present at the 26th MK-Equity Investment Conference, hosted by MK-Equity, the family office of Michael Kott, on Wednesday, September 30th, 2026, in Munich, Germany. The conference, a by-invitation-only gathering of family offices, high-net-worth individuals, active investors, and entrepreneurs, aims to connect like-minded investors around a range of megatrends.
Bruce Bragagnolo, CEO of Regency Silver, will present the company's equity story directly to the conference audience, providing updates on its Dios Padre and Jabali projects. The Dios Padre Project in Yecora, Sonora, Mexico, has seen significant exploration success, with high-grade intercepts including: - REG-23-21: 38 metres of 7.36 g/t gold - REG-26-35: 36 metres of 5.06 g/t gold, 1.1% copper, and 42.85 g/t silver - REG-22-01: 36 metres of 6.84 g/t gold, 0.88% copper, and 21.8 g/t silver - REG-23-14: 29.4 metres of 6.32 g/t gold
A NI 43-101 Technical Report, dated March 2, 2023, prepared by Gordon Gibson, B.Sc., P.Geo, estimates an inferred mineral resource of 11.375 million ounces of silver equivalent, calculated as 1.384 million tonnes at 255.64 g/t AgEq. This report does not include the above results.
Recently, Regency Silver announced an agreement to acquire the past-producing La Dura gold mine, located only 20 km from Dios Padre and 6 km from the Mulatos mine. This acquisition further strengthens Regency Silver's position in the region and expands its portfolio of high-grade mineral assets.
Regency Silver Corp. (TSXV: RSMX) (OTCQB: RSMXF) (FSE: ZJ90) is a Canadian mineral exploration company focused on high-grade gold, silver, and copper in Mexico. The Company's flagship asset is the Dios Padre Project in Yecora, Sonora, Mexico, where Regency Silver has discovered a large, high-grade gold-copper-silver system interpreted as a magmatic-hydrothermal breccia that widens with depth.