Reference Type | Conference Paper/Abstract |
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Title | The Trapiche Ni-Co prospect, Yauli Dome, Central Peru: formed by Miocene magmatic-hydrothermal activity |
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Conference | pro explo 2021 |
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Authors | Martínez, Alvaro | Author |
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Fontboté, Lluís | Author |
Spangenberg, Jorge | Author |
Angeles, Carlos | Author |
Farfán, César | Author |
Year | 2021 |
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Classification | Not set | LoC | Not set |
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Mindat Ref. ID | 18462247 | Long-form Identifier | mindat:1:5:18462247:4 |
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GUID | 0 |
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Full Reference | Martínez, Alvaro; Fontboté, Lluís; Spangenberg, Jorge; Angeles, Carlos; Farfán, César (2021) The Trapiche Ni-Co prospect, Yauli Dome, Central Peru: formed by Miocene magmatic-hydrothermal activity. pro explo 2021. |
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Plain Text | Martínez, Alvaro; Fontboté, Lluís; Spangenberg, Jorge; Angeles, Carlos; Farfán, César (2021) The Trapiche Ni-Co prospect, Yauli Dome, Central Peru: formed by Miocene magmatic-hydrothermal activity. pro explo 2021. |
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Abstract/Notes | The Trapiche Ni-Co prospect, province of Yauli, is located in the SE tip of the Yauli Dome, 2 km SE of the Andaychagua Ag-Zn-Pb mine. At Trapiche, discontinuous Ni-Co-Zn-Pb-Cu manto bodies are hosted by weakly metamorphic carbonate and basaltic rocks of the Devonian Excelsior Group. Despite its Ni-Co rich mineral association, Trapiche shares main characteristics with Miocene Cordilleran polymetallic deposits in the area. |
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