Faulting migration and localization at fast extension rates during rifting of the Tyrrhenian Basin have lead to break up and mantle exhumation
American Geophysical Union (AGU) Fall Meeting, 9-13 December 2013, San Francisco
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Main Authors: | , , , , , |
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Format: | comunicación de congreso biblioteca |
Language: | English |
Online Access: | http://hdl.handle.net/10261/98281 |
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