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- W20002856 abstract "The Patagonian Andes are di~ided into the External and Internal Tectonic Domains. The External Tectonic Domain is characterized by structures developed in the sedimentary cover, scarce basement outcrops, low temperature deformation (usually not above green schist facies) and almost absent calcalcaline magmatism. The Internal Tectonic Domain is characterized by low to high grade polydeformed metamorphic rocks emplaced as basement thrust sheets, basic rocks with oceanic crust affinities, and abundant calcalkaline magmatism. These two descriptive domains can be mapped regionally and the boundary is a transitional zone with basement thrust-and basement cored anticlines. Here I show a regional balanced cross section through the Patagonian Andes which goes from Tierra del Fuego island to the Pacific ocean (Figure I-A). It was constructed using the faultbend folding theory [Suppe, 19851. The cross section presents a new interpretation linking the structures of the External and Internal domains. The rocks of the Internal domain are interpreted as alocthonous thrust sheets transported hundreds of kilometers along a basal decollement. The deformation propagates from the Internal to the External domain since Mid Cretaceous to Cenozoic." @default.
- W20002856 created "2016-06-24" @default.
- W20002856 creator A5089004977 @default.
- W20002856 date "1996-01-01" @default.
- W20002856 modified "2023-09-27" @default.
- W20002856 title "Regional balanced cross section in the Patagonian Andes of Tierra del Fuego (Argentina and Chile)" @default.
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