お知らせ • Oct 09
Mundoro Capital Inc. Identifies Large-Scale Porphyry Targets in Timok Properties, Serbia
Mundoro Capital Inc. announced that it has identified four highly prospective porphyry exploration targets at the Tilva Rosh prospect area on Mundoro's 100% owned licenses. These targets include: Tilva Rosh Valley: A 2 km x 2 km target area located at the junction of two significant fault structures, identified through geophysics, structural interpretation and geochemical data. Tilva Rosh North: A 3 km x 1.5 km target featuring advanced surface alteration and increasing molybdenum grades at depth, indicating potential deeper sulfide-rich porphyry zones. Tilva Rosh South: A deeper porphyry target identified through previous drilling, which demonstrated molybdenum anomalies at depth and porphyry style alteration zonation. Tilva Rosh Bridge: A 2.3 km zone linking two lithocaps, with elevated copper-gold soil anomalies and geophysical indicators suggesting potential for porphyry system. The Tilva Rosh lithocap, covering approximately 16 square kilometers, is situated in the central part of the Timok Magmatic Complex, near the highly productive Bor and Cukaru Peki Mine Complexes. Through exploration work, identified four promising target areas: Tilva Rosh Valley, Tilva Rosh North, Tilva Rosh South, and Tilva Rosh Bridge. These targets show similarities to the Bor and Cukaru Peki deposits, not only in geological features but also in mineralization styles, and alteration patterns that often signal the presence of porphyry and high-sulphidation epithermal (HSE) systems. Tilva Rosh Valley: This 2 km x 2 km target area is centered on a significant fault system concealed beneath alluvial cover, identified through a combination of geophysical and structural interpretation. The area is a structurally significant dilation zone, which could trap mineralizing fluids, creating favorable conditions for porphyry development. Located just north of a 4 km long lithocap, this area is likely the extension under cover of that lithocap, supported by the continuation of a demagnetized zone as indicated by geophysical surveys. Key porphyry indicators, including surface molybdenum anomalies, demagnetization, and structural interpretation, coupled with a new passive seismic survey, suggest potential for a porphyry- related system. Two drill holes have been designed to test for both porphyry and the associated high-sulphidation epithermal (HSE) systems, guided by molybdenum anomalies, magnetics, and passive seismic data that align with the area's structural trends. Tilva Rosh North: This expansive lithocap (4 km by 2 km) is characterized by advanced surface alteration, with argillic and albite-sericite-chlorite zones transitioning into anhydrite at depth. Increasing molybdenum grades to the north and deeper levels, along with magnetic highs within broader demagnetization zones, suggest potential for a sulfide-rich potassic zone in a deeper porphyry system. Traditional porphyry vectors such as A-type quartz-magnetite veinlets further support the potential for mineralization at depth. Two drill holes have been designed to test this area, targeting porphyry and related HSE systems using geophysical data, including magnetic highs and geochemical anomalies, which provide strong evidence for mineralization in this promising target. The southern end of the lithocap presents a deeper target for porphyry systems, as near surface drilling has not fully explained the widespread surface alteration and high-grade mineralization from channel sampling which returned 12m @ 30.39 g/t Au and 171.27 g/t Ag. Molybdenum anomalies, both at the surface and along one hole previously drilled in this area, along with alteration zonation and A-type quartz-magnetite veinlets, are vectors pointing toward a deeper porphyry system. A single deep drill hole (FMSC18006) revealed extensive alteration, including hydrothermal breccia and potassic-altered diorite porphyry, indicating the potential for substantial mineralization at depth. One drill hole has been designed to further test this deeper potential, guided by these vectors and supported by geochemical, magnetic, and structural indicators from previous drilling.