3-D numerical model of the flexural isostatic response to extension induced by crustal scale listric normal faulting
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| Format: | Artículo científico |
| Language: | en |
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Universidad Nacional Autónoma de México
2003
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| author | Juan García Abdeslem |
| author_facet | Juan García Abdeslem |
| contents | 3-D numerical model of the flexural isostatic response to extension induced by crustal scale listric normal faulting Juan García Abdeslem Ciencias de la Tierra Isostasy crustal extension 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 state under the action of applied loads provides simple analytical expressions forcomputing the flexural isostatic response 3-D. An example using an analytically defined curvilinear normal fault is provided. 2003 artículo científico 0016-7169 https://www.redalyc.org/articulo.oa?id=56842103 en http://www.redalyc.org/revista.oa?id=568 Geofísica Internacional application/pdf Universidad Nacional Autónoma de México Geofísica Internacional (México) Num.1 Vol.42 |
| format | Artículo científico |
| id | redalyc_56842103 |
| institution | Redalyc |
| language | en |
| publishDate | 2003 |
| publisher | Universidad Nacional Autónoma de México |
| spellingShingle | 3-D numerical model of the flexural isostatic response to extension induced by crustal scale listric normal faulting Juan García Abdeslem Ciencias de la Tierra Isostasy crustal extension listric normal faulting 3-D numerical model of the flexural isostatic response to extension induced by crustal scale listric normal faulting Juan García Abdeslem Ciencias de la Tierra Isostasy crustal extension 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 state under the action of applied loads provides simple analytical expressions forcomputing the flexural isostatic response 3-D. An example using an analytically defined curvilinear normal fault is provided. 2003 artículo científico 0016-7169 https://www.redalyc.org/articulo.oa?id=56842103 en http://www.redalyc.org/revista.oa?id=568 Geofísica Internacional application/pdf Universidad Nacional Autónoma de México Geofísica Internacional (México) Num.1 Vol.42 |
| title | 3-D numerical model of the flexural isostatic response to extension induced by crustal scale listric normal faulting |
| topic | Ciencias de la Tierra Isostasy crustal extension listric normal faulting |
| url | https://www.redalyc.org/articulo.oa?id=56842103 |