Terranes and tectonic evolution of the Andes: A regional synthesis.
The Pacific margin of South America was predominantly a subduction margin throughout the Mesozoic and Cenozoic. In the mid-Cretaceous, the continental margin arc from southernmost South America to southern Peru changed from a near sea-level, "neutral" arc to a subaerial, compressive arc. O...
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| Language: | en |
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The University of Arizona.
1995
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| Online Access: | http://hdl.handle.net/10150/187114 |