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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Main Authors: Wernicke, B, Christiansen, R, England, P, Sonder, L
Other Authors: Coward, M
Format: Journal article
Language:English
Published: 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
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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
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AT christiansenr tectonomagmaticevolutionofcenozoicextensioninthenorthamericacordillera
AT englandp tectonomagmaticevolutionofcenozoicextensioninthenorthamericacordillera
AT sonderl tectonomagmaticevolutionofcenozoicextensioninthenorthamericacordillera