3-D numerical model of the flexural isostatic response to extension induced by crustal scale listric normal faulting
The flexural isostatic response of the lithosphere, induced by listric normal faulting, is modeled by assuming that simpleshearextension takes place in the brittle upper crust while the lower crust and upper mantle extend in pure shear. The partialdifferential equation describing the equilibrium sta...
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| Publicado no: | Geofísica Internacional |
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| Autor principal: | |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Universidad Nacional Autónoma de México
2003
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| Assuntos: | |
| Acesso em linha: | https://www.redalyc.org/articulo.oa?id=56842103 |
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