Tectonomagmatic evolution of Cenozoic extension in the North America Cordillera.
The spatial and temporal distributions of Cenozoic extension and magmatism in the Cordillera suggest that the onset of major crustal extension at a particular latitude was confined to a relatively narrow belt (<100 km, pre-extension) and followed the onset of intermediate and silicic magmatis...
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Format: | Journal article |
Language: | English |
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Blackwell Scientific; Geological Society Special Publication, 28
1987
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author | Wernicke, B Christiansen, R England, P Sonder, L |
author2 | Coward, M |
author_facet | Coward, M Wernicke, B Christiansen, R England, P Sonder, L |
author_sort | Wernicke, B |
collection | OXFORD |
description | The spatial and temporal distributions of Cenozoic extension and magmatism in the Cordillera suggest that the onset of major crustal extension at a particular latitude was confined to a relatively narrow belt (<100 km, pre-extension) and followed the onset of intermediate and silicic magmatism by no more than a few Ma. We recognize a correlation between the amount of earlier crustal thickening and Cenozoic extension, and between the length of time after shortening but before extension and the degree to which a given region was intruded by Late Cretaceous plutons.-from Authors |
first_indexed | 2024-03-06T23:42:04Z |
format | Journal article |
id | oxford-uuid:6fa7ad30-e2ac-48b6-a72f-231f7b248251 |
institution | University of Oxford |
language | English |
last_indexed | 2024-03-06T23:42:04Z |
publishDate | 1987 |
publisher | Blackwell Scientific; Geological Society Special Publication, 28 |
record_format | dspace |
spelling | oxford-uuid:6fa7ad30-e2ac-48b6-a72f-231f7b2482512022-03-26T19:32:10ZTectonomagmatic evolution of Cenozoic extension in the North America Cordillera.Journal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:6fa7ad30-e2ac-48b6-a72f-231f7b248251EnglishSymplectic Elements at OxfordBlackwell Scientific; Geological Society Special Publication, 281987Wernicke, BChristiansen, REngland, PSonder, LCoward, MDewey, JHancock, PThe spatial and temporal distributions of Cenozoic extension and magmatism in the Cordillera suggest that the onset of major crustal extension at a particular latitude was confined to a relatively narrow belt (<100 km, pre-extension) and followed the onset of intermediate and silicic magmatism by no more than a few Ma. We recognize a correlation between the amount of earlier crustal thickening and Cenozoic extension, and between the length of time after shortening but before extension and the degree to which a given region was intruded by Late Cretaceous plutons.-from Authors |
spellingShingle | Wernicke, B Christiansen, R England, P Sonder, L Tectonomagmatic evolution of Cenozoic extension in the North America Cordillera. |
title | Tectonomagmatic evolution of Cenozoic extension in the North America Cordillera. |
title_full | Tectonomagmatic evolution of Cenozoic extension in the North America Cordillera. |
title_fullStr | Tectonomagmatic evolution of Cenozoic extension in the North America Cordillera. |
title_full_unstemmed | Tectonomagmatic evolution of Cenozoic extension in the North America Cordillera. |
title_short | Tectonomagmatic evolution of Cenozoic extension in the North America Cordillera. |
title_sort | tectonomagmatic evolution of cenozoic extension in the north america cordillera |
work_keys_str_mv | AT wernickeb tectonomagmaticevolutionofcenozoicextensioninthenorthamericacordillera AT christiansenr tectonomagmaticevolutionofcenozoicextensioninthenorthamericacordillera AT englandp tectonomagmaticevolutionofcenozoicextensioninthenorthamericacordillera AT sonderl tectonomagmaticevolutionofcenozoicextensioninthenorthamericacordillera |