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Location: 10 km NE from El Melon, Chile
Pedro de Valdivia 291 ProvidenciaSantiagoChile
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Anglo American Sur S.A. shareholders: Anglo American plc (50.1%), Joint Venture between Chile’s state-run copper producer Corporación Nacional del Cobre de Chile and Mitsui & Co., Ltd. (29.5%), Mitsubishi Corporation (20.4%).
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El Soldado, located in Central Chile 120 km northwest of Santiago, is the largest (>200 Mt @ 1.4 % Cu) of the known copper manto-type deposits in central Chile. El Soldado is a copper manto-type deposit that is regionally strata-bound within volcanic rocks of the Lower Cretaceous Lo Prado Formation. Locally, the mineralisation is discordant with the strata and controlled by trachytic (rhyodacite) feeders, trachytic flows and fault intersections. The orebodies are irregular in shape and size, and show an outer pyrite-rich halo, followed inwards by chalcopyritic zones and a bornite-chalcocite core. The mineralisation is mainly primary and is discordant with the host strata.Although structurally controlled and discordant at the scale of the mine, it is regionally strata-bound within shallow marine, bimodal calc-alkaline basalt - rhyodacite (extrusive- intrusive) rocks of the Lower Cretaceous Lo Prado Formation, which also contains marine carbonaceous shale and volcaniclastic sandstones. It is generally acknowledged that hydrothermal sulphide base metal deposits in the Andes obtained their metals and sulfur from calc-alkaline magmatic systems. Several structurally-controlled orebody clusters occur within an area of ca. 2000 x 800 m, 600 m vertical, in a dilational fault jog within a large NS orogen parallel (sinistral) strikeslip shear fault system that was active in the Cretaceous. The orebodies are zoned with pyrite in outer halos or envelopes, followed inwards by zones with abundant pyrite-chalcopyrite, chalcopyrite-bornite and a bornite-chalcocite core with minor hematite in the higher levels and the chalcocite cores; pyrite is relatively more abundant at depth and in the northern half of the deposit.Samples of massive pyrite and associated chalcopyrite and bornite, devoid of visible bitumen, were selected from the Valdivia Sur, Arauco Norte, Catedral and Morro orebody clusters, most from the pyrite-chalcopyrite halos such as those shown in, or veins. Under close inspection under the reflected microscope and the microprobe, even the most massive pyrite assemblages show remnants of colloidal or framboidal textures. As temperature rose, framboidal structures recrystallized as cubes, yet (at high magnification) their cores preserve the diagenetic framboidal structures. Partial or total replacement of pyrite by chalcopyrite and bornite did not totally destroy the original diagenetic textures.
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