Seismic ridge subduction and topography: Foreland deformation in the Patagonian Andes
The Patagonian Andes recorded several episodes of active ridge subduction in the last 80 million years. An analysis of the spatial and temporal relation between the present segment of collision of the Chile ridge and the digital topography of the foreland shows a correlation with the beginning of de...
Published in: | Tectonophysics |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
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Elsevier Science
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Online Access: | http://hdl.handle.net/11336/92808 |