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Stable isotope (C, O) constraints on the genesis of the Mississippi Valley-type zinc-lead deposit of San Vicente, central Peru

Presented atConcepción, 17-21 octubre de 1994
Published inUniversidad de Concepción (Chile). Departamento Ciencias de la Tierra (Ed.), 7° Congreso Geológico Chileno: actas, p. 1532-1536
PublisherConcepción : Universidad de Concepción. Departamento Ciencias de la Tierra
Publication date1994
Abstract

The Mississippi Valley-type (MVT) Zn-Pb district of San Vicente is located in central Peru (300 km east of Lima) within the carbonate rocks of the Triassic-Jurassic Pucara basin. Detailed carbon and oxygen isotope studies of the carbonates and associated organic matter from the main deposit and minor ore-occurrences provide new insights on the mechanism of ore-precipitation in San Vicente. The regional homogeneity of the isotopic composition of the altered host and gangue carbonates, coupled with the strong mineralogical and petrographic similarities of the distinct MVT-occurrences reflects that the mineralizing processes were similar in the whole San Vicente belt, suggesting the existence of a regional mineralizing hydrothermal system with interconnected plumbing.

Citation (ISO format)
SPANGENBERG, Jorge Enrique et al. Stable isotope (C, O) constraints on the genesis of the Mississippi Valley-type zinc-lead deposit of San Vicente, central Peru. In: 7° Congreso Geológico Chileno: actas. Universidad de Concepción (Chile). Departamento Ciencias de la Tierra (Ed.). Concepción. Concepción : Universidad de Concepción. Departamento Ciencias de la Tierra, 1994. p. 1532–1536.
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