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Mantos Blancos is a copper-silver deposit located in the Coastal Range of northern Chile, which is an important geomorphological feature because it hosts Cu-Ag-Au stratabound deposits along an early Cretaceous metallogenic belt.
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Mantos Blancos es un yacimiento de cobre y plata ubicado en...
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22 de abr. de 2006 · The Upper Jurassic Mantos Blancos copper deposit (500 Mt at 1.0% Cu), located in the Coastal Range of northern Chile, displays two superimposed hydrothermal events.
Mantos Blancos es un yacimiento de cobre y plata ubicado en la Cordillera de la Costa del norte de Chile, que es una característica geomorfológica importante porque alberga yacimientos estratificados de Cu-Ag-Au a lo largo de un cinturón metalogénico del Cretácico temprano.
The Upper Jurassic Mantos Blancos copper deposit (500 Mt at 1.0% Cu), located in the Coastal Range of northern Chile, displays two superimposed hydrother-mal events. An older phyllic alteration probably related to felsic magmatic hydrothermal brecciation at ∼155 Ma, and.
The Upper Jurassic Mantos Blancos copper deposit (500 Mt at 1.0% Cu), located in the Coastal Range of northern Chile, displays two superimposed hydrothermal events.
1 de may. de 2001 · Description and evolution of the escondida porphyry copper deposit.
The deposit of Jurassic Volcanic rocks is a magmatic hydrothermal breccia-style copper deposit. It exhibits two superimposed hydrothermal events. The first mineralisation event is associated with a phyllic hydrothermal alteration affecting a rhyolitic dome.
