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Mapa Interactivo (Tipo Besshi/Tipo Kuroko)

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En este mapa deberan ubicar el tipo de despósito correspondiente al contexto tectónico (Tipo Beshhi o tipo Kuroko)

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Chile

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Mapa Interactivo (Tipo Besshi/Tipo Kuroko)
 

Mapa Interactivo (Tipo Besshi/Tipo Kuroko)Online version

En este mapa deberan ubicar el tipo de despósito correspondiente al contexto tectónico (Tipo Beshhi o tipo Kuroko)

by Sebastián Godoy Ardiles
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Explicación

Los depósitos Tipo Besshi se forman en cuencas marinas profundas con alta sedimentación (turbiditas) intercalada con lavas basálticas (sills o flujos). A diferencia del tipo Chipre (que es pura corteza oceánica), el Besshi requiere este entorno sedimentario de rifting o trasarco

Los depósitos Tipo Kuroko están vinculados a magmas félsicos (riolitas/dacitas) en arcos volcánicos. Son famosos por ser polimetálicos y de alta ley: contienen una mezcla económica de Cobre (Cu), Zinc (Zn), Plomo (Pb), Plata (Ag) y Oro (Au)

Tipo Kuroko se forma en la superficie del fondo marino. El agua de mar se infiltra, se calienta, disuelve metales de las rocas y luego es expulsada violentamente hacia arriba (fumarolas negras).

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