EXTENSION DURING CONTINENTAL CONVERGENCE, WITH APPLICATION TO THE TIBETAN PLATEAU
The Tibetan plateau is the product of crustal thickening caused by the collision between India and Asia and is the largest active example of extensional tectonics in a zone of continental collision. Throughout most of the Tertiary, the tectonics of the plateau were dominated by north-south shortenin...
| Autores principales: | , |
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| Formato: | Journal article |
| Lenguaje: | English |
| Publicado: |
1989
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| _version_ | 1826258126304706560 |
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| author | England, P Houseman, G |
| author_facet | England, P Houseman, G |
| author_sort | England, P |
| collection | OXFORD |
| description | The Tibetan plateau is the product of crustal thickening caused by the collision between India and Asia and is the largest active example of extensional tectonics in a zone of continental collision. Throughout most of the Tertiary, the tectonics of the plateau were dominated by north-south shortening, a significant proportion of which took place on east-west striking thrust faults. For the last 5 m.a. or so the plateau has been thinning by the mechanism of extension on north-south trending normal faults. Previous investigations of the collision have been able to account for the large-scale features of the Tertiary deformation but have failed to explain the transition, in the late Tertiary to Quaternary strain rate field of the plateau, from north-south compression to east-west extension. The transition could, in principle, be effected by a reduction in the rate of convergence between India and Asia or by a uniform reduction in strength of the whole continental lithosphere of Asia. Numerical experiments show that for a range of lithospheric parameters, the increase in surface height (as much as 2 km) and of potential energy (5 to 10 × 1012 N m-1) resulting from convective instability of the lower lithosphere are sufficient for east-west extension to replace north-south compression as the dominant feature of the stress field of the Tibetan plateau. -from Authors |
| first_indexed | 2024-03-06T18:29:06Z |
| format | Journal article |
| id | oxford-uuid:0903524e-7f43-455c-9d21-34ceca9940ac |
| institution | University of Oxford |
| language | English |
| last_indexed | 2024-03-06T18:29:06Z |
| publishDate | 1989 |
| record_format | dspace |
| spelling | oxford-uuid:0903524e-7f43-455c-9d21-34ceca9940ac2022-03-26T09:15:56ZEXTENSION DURING CONTINENTAL CONVERGENCE, WITH APPLICATION TO THE TIBETAN PLATEAUJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:0903524e-7f43-455c-9d21-34ceca9940acEnglishSymplectic Elements at Oxford1989England, PHouseman, GThe Tibetan plateau is the product of crustal thickening caused by the collision between India and Asia and is the largest active example of extensional tectonics in a zone of continental collision. Throughout most of the Tertiary, the tectonics of the plateau were dominated by north-south shortening, a significant proportion of which took place on east-west striking thrust faults. For the last 5 m.a. or so the plateau has been thinning by the mechanism of extension on north-south trending normal faults. Previous investigations of the collision have been able to account for the large-scale features of the Tertiary deformation but have failed to explain the transition, in the late Tertiary to Quaternary strain rate field of the plateau, from north-south compression to east-west extension. The transition could, in principle, be effected by a reduction in the rate of convergence between India and Asia or by a uniform reduction in strength of the whole continental lithosphere of Asia. Numerical experiments show that for a range of lithospheric parameters, the increase in surface height (as much as 2 km) and of potential energy (5 to 10 × 1012 N m-1) resulting from convective instability of the lower lithosphere are sufficient for east-west extension to replace north-south compression as the dominant feature of the stress field of the Tibetan plateau. -from Authors |
| spellingShingle | England, P Houseman, G EXTENSION DURING CONTINENTAL CONVERGENCE, WITH APPLICATION TO THE TIBETAN PLATEAU |
| title | EXTENSION DURING CONTINENTAL CONVERGENCE, WITH APPLICATION TO THE TIBETAN PLATEAU |
| title_full | EXTENSION DURING CONTINENTAL CONVERGENCE, WITH APPLICATION TO THE TIBETAN PLATEAU |
| title_fullStr | EXTENSION DURING CONTINENTAL CONVERGENCE, WITH APPLICATION TO THE TIBETAN PLATEAU |
| title_full_unstemmed | EXTENSION DURING CONTINENTAL CONVERGENCE, WITH APPLICATION TO THE TIBETAN PLATEAU |
| title_short | EXTENSION DURING CONTINENTAL CONVERGENCE, WITH APPLICATION TO THE TIBETAN PLATEAU |
| title_sort | extension during continental convergence with application to the tibetan plateau |
| work_keys_str_mv | AT englandp extensionduringcontinentalconvergencewithapplicationtothetibetanplateau AT housemang extensionduringcontinentalconvergencewithapplicationtothetibetanplateau |