Subduction of the Nazca Ridge and the Inca Plateau: Insights into the formation of ore deposits in Peru
2005
Rosenbaum, G. | Giles, D. | Saxon, M. | Betts, P. | Weinberg, R. | Duboz, C.
A large number of ore deposits that formed in the Peruvian Andes during the Miocene (15-5 Ma) are related to the subduction of the Nazca plate beneath the South American plate. Here we show that the spatial and temporal distribution of these deposits correspond with the arrival of relatively buoyant topographic anomalies, namely the Nazca Ridge in central Peru and the now-consumed Inca Plateau in northern Peru, at the subduction zone. Plate reconstruction shows a rapid metallogenic response to the arrival of the topographic anomalies at the subduction trench. This is indicated by clusters of ore deposits situated within the proximity of the laterally migrating zones of ridge subduction. It is accordingly suggested that tectonic changes associated with impingement of the aseismic ridge into the subduction zone may trigger the formation of ore deposits in metallogenically fertile suprasubduction environments. © 2005 Elsevier B.V. All rights reserved.
显示更多 [+] 显示较少 [-]Gideon Rosenbaum, David Giles, Mark Saxon, Peter G. Betts, Roberto F. Weinberg and Cecile Duboz
显示更多 [+] 显示较少 [-]http://www.elsevier.com/wps/find/journaldescription.cws_home/503328/description#description
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