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Location: 9 km NE from Cosala, Sinaloa, Mexico
Belisario Domínguez No. 29 a Cosalá cruzar las comunidades de la Estancia y los BracerosCosaláSinaloa, Mexico80700
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Zone 120 in the eastern portion of the San Rafael deposit contains silver-copper mineralization within garnet-pyroxene-calcite skarn. The strong metasomatic alteration and the close spatial relationship with a large dioritic intrusion suggest that Zone 120 represents a proximal skarn deposit. El Cajón is a proximal silver-copper skarn related to an adjacent nearly cylindrical diorite intrusive body. Mineralization at El Cajón is replacement type and occurs as horizons in recrystallized limestone which are connected by mineralized zones localized by steeply dipping contacts, faults and fractures.Zone 120 occurs not as a single horizon, but as multiple bedding- and intrusive-contact-related mineralized horizons. As currently defined, the Zone 120 mineralization occurs within a rock volume that is approximately 600m long, 250m wide and extends to a depth of about 350m below the surface. It strikes in a direction of 330°, and below the massive sulphide, the bedding-related mineralization dips steeply to the northeast at approximately 50°. The Zone 120 mineralization is interpreted to occur along near-vertical contacts between diorite and skarn-altered lime rich volcarenites in the lower parts, and in quartz-sericite-pyrite-altered volc-arenites in the upper portions. The quartz altered material is now referred to as hornfels, differing from earlier interpretations. Hornfels seems to be developed in carbonate poor rocks whereas the more highly mineralized skarn is developed in more carbonate rich rocks. Carbonate content is judged based on fragments and inclusions with the Va2 or volc-arenite package. The Zone 120 mineralization extends upwards to overlap with the San Rafael Main Zone mineralization. Mineralization is associated with generally 2 to 10% sulphides and is more irregular in shape and more variable in mineral character than the San Rafael Main Zone. It consists of silver-copper-gold mineralization in the form of chalcopyrite and tetrahedrite with minor pyrite, galena, sphalerite, arsenopyrite, chalcocite, jalpaite, native silver, copper and bismuth. This mineralization accompanies pyroxene-garnet-calcite skarn alteration. Mineralization is best developed in unit Va2, a volcarenite with a high component of carbonaceous fragments and carbonate. These are contained with beds of the same unit which a more siliceous and from hornfels instead of calcareous skarn. The hornfels are not a favourable host generally. Both skarn alteration and sulphide mineralization are spatially associated with intermediate dikes, sills and small stocks.El Cajón mineralization consists of mantos and chimneys developed in skarn and recrystallized limestone. El Cajón and Zone 120 mineralization are similar in character consisting of veinlets and replacements of chalcopyrite and tetrahedrite-tennantite. The El Cajón deposit is roughly oval shaped extending 550m east-west and 400m north-south, with the mineralization aligned along the general 330° strike and 20° northeast dip of the limestone country rock. It varies in depth from approximately 20m below surface to a depth of approximately 250m.
