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Location: 67 km NE from Durango, Durango, Mexico
Alonso de Pacheco 300Nueva VizcayaDurangoDurango, Mexico34080
Stay on top of the latest gold discoveries. Examine the latest updates on drilling outcomes spanning various commodities.
Mining scale, mining and mill throughput capaciites.Full profiles of select mines and projects.
Shaft depth, mining scale, backfill type and mill throughput data.Full profiles of select mines and projects.
Equipment type, model, size and quantity.Full profiles of select mines and projects.
Camp size, mine location and contacts.Full profiles of select mines and projects.
The property ownership is distributed as follows: CMMA (subsidiary) holds 98.45%, Promotora Avino, S.A. de C.V. (subsidiary) owns 1.22%, and the Estate of Ysita holds a non-controlling interest of 0.33%.
The San Gonzalo Vein system, including the crosscutting Angelica Vein, is located 2 km northeast of the Avino Vein. It constitutes a strongly developed vein system over 25 m across, trending 300° to 325°/80° northeast to 77° south. Banded textures and open-space filling are common, and individual veins have an average width of less than 2 m. The vein was mined historically, and underground workings extend approximately 1.1 km along the strike to the 1,970 masl (300 m below the surface).The San Gonzalo is a typical narrow vein, precious metal deposit with some erratic values and extends approximately 2 km to the northwest to the Santa Ana-Malinche area (Gunning 2009).The Cerro San Jose-La Estella-San Gonzalo Cerro San Jose represents a distinct hydrothermal centre with similar characteristics to the Avino system, which include the following (Paulter 2006):• Occur on a topographic high.• Strong to intense silicification and brecciation.• Easterly trending stockwork system similar to the trend of the Avino Vein.• Similar temperatures of formation to Avino.• Presence of an intersecting northwesterly trending vein system (la Estella at San Jose and San Juventino at Avino).• Emplacement along a northerly trending, deep crustal fault zone (defined by the Aguila Mexicana Vein at Cerro San Jose and the felsic dyke at Avino).
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