3-D numerical model of the flexural isostatic response to extension induced by crustal scale listric normal faulting

3-D numerical model of the flexural isostatic response to extension induced by crustal scale listric normal faulting

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The flexural isostatic response of the lithosphere, induced by listric normal faulting, is modeled by assuming that simple-shear extension takes place in the brittle upper crust while the lower crust and upper mantle extend in pure shear. The partial differential equation describing the equilibrium...

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Bibliographic Details
Main Author:	Juan García Abdeslem
Format:	Article
Language:	English
Published:	Universidad Nacional Autónoma de México, Instituto de Geofísica 2003-01-01
Series:	Geofísica Internacional
Subjects:	Isostasy crustal extension listric normal faulting.
Online Access:	http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2003/01/garcia.pdf

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