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- W1755291386 abstract "Structural control on Neogene volcanism and related ore deposits at Canada Honda District, San Luis province. Located at the transitional southern end (33° S) of the Pampean flat-slab, the records the eastward migration of the Andean volcanic arc due to the flattening of the Nazca Plate in Mio-Pliocene times. The tertiary volcanic belt encompasses several very important me- tallogenetic districts in the San Luis Pampean Ranges. Volcanic rocks and associated ore-deposits crop out following a NW- WNW trending belt at La Carolina, Canada Honda - Cerros Largos, Cerros del Rosario and El Morro volcanic fields. The available geochronological data indicate that the volcanic activity began early at the western end of the belt and ended ~ 10 Ma later at its eastern border. Canada Honda district represents the oldest and longest-lived volcanic field of the tertiary vol- canic belt. It records eruptive events and related hydrothermal alteration from 12-13 Ma to 7.3 Ma, including lavas and volca- niclastic products. Preliminary structural analysis shows that previous structures have strongly controlled, either directly or in- directly, the emplacement of volcanic rocks and related mineral deposits. Kinematic and strain fabric analyses allow to recog- nize two volcano-tectonic associations. One of these associations would be related to dextral reactivations of structures pa- rallel to basement foliation. On the other hand, the main one would be linked with the generation of two volcano-tectonic depressions which are aligned in a NW-WNW direction. Their dominant structures trend NW-WNW and reveal sinistral-nor- mal motions, both at local and TVB scales." @default.
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- W1755291386 date "2010-12-01" @default.
- W1755291386 modified "2023-09-26" @default.
- W1755291386 title "Control estructural en el emplazamiento del volcanismo y mineralizaciones neógenas, distrito Cañada Honda, San Luis" @default.
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