Circum-Pacific mid-Cretaceous deformation and uplift: A superplume-related event?
Evidence of short-lived episodes of mid-Cretaceous deformation, metamorphism, uplift, and hiatus in sedimentation is widespread in the Lower Cretaceous rocks that bordered the Cretaceous Pacific basin. I present a model in which these coeval but widely spaced events are linked to increased ridge-pus...
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ftnerc:oai:nora.nerc.ac.uk:515878 2023-05-15T13:49:33+02:00 Circum-Pacific mid-Cretaceous deformation and uplift: A superplume-related event? Vaughan, Alan P.M. 1995 http://nora.nerc.ac.uk/id/eprint/515878/ https://doi.org/10.1130/0091-7613(1995)023<0491:CPMCDA>2.3.CO;2 unknown Geological Society of America Vaughan, Alan P.M. 1995 Circum-Pacific mid-Cretaceous deformation and uplift: A superplume-related event? Geology, 23 (6). 491-494. https://doi.org/10.1130/0091-7613(1995)023<0491:CPMCDA>2.3.CO;2 <https://doi.org/10.1130/0091-7613(1995)023<0491:CPMCDA>2.3.CO;2> Publication - Article PeerReviewed 1995 ftnerc https://doi.org/10.1130/0091-7613(1995)023<0491:CPMCDA>2.3.CO;2 2023-02-04T19:44:17Z Evidence of short-lived episodes of mid-Cretaceous deformation, metamorphism, uplift, and hiatus in sedimentation is widespread in the Lower Cretaceous rocks that bordered the Cretaceous Pacific basin. I present a model in which these coeval but widely spaced events are linked to increased ridge-push force at subduction zones triggered by large-scale upwelling of mantle associated with the mid-Cretaceous superplume. This model can account for mid-Cretaceous terrane accretion and ophiolite obduction events and can explain brief compressional phases in predominantly extensional orogenies as recognized in Alaska, British Columbia, California, western South America, and West Antarctica. Article in Journal/Newspaper Antarc* Antarctica West Antarctica Alaska Natural Environment Research Council: NERC Open Research Archive Pacific West Antarctica |
institution |
Open Polar |
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Natural Environment Research Council: NERC Open Research Archive |
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ftnerc |
language |
unknown |
description |
Evidence of short-lived episodes of mid-Cretaceous deformation, metamorphism, uplift, and hiatus in sedimentation is widespread in the Lower Cretaceous rocks that bordered the Cretaceous Pacific basin. I present a model in which these coeval but widely spaced events are linked to increased ridge-push force at subduction zones triggered by large-scale upwelling of mantle associated with the mid-Cretaceous superplume. This model can account for mid-Cretaceous terrane accretion and ophiolite obduction events and can explain brief compressional phases in predominantly extensional orogenies as recognized in Alaska, British Columbia, California, western South America, and West Antarctica. |
format |
Article in Journal/Newspaper |
author |
Vaughan, Alan P.M. |
spellingShingle |
Vaughan, Alan P.M. Circum-Pacific mid-Cretaceous deformation and uplift: A superplume-related event? |
author_facet |
Vaughan, Alan P.M. |
author_sort |
Vaughan, Alan P.M. |
title |
Circum-Pacific mid-Cretaceous deformation and uplift: A superplume-related event? |
title_short |
Circum-Pacific mid-Cretaceous deformation and uplift: A superplume-related event? |
title_full |
Circum-Pacific mid-Cretaceous deformation and uplift: A superplume-related event? |
title_fullStr |
Circum-Pacific mid-Cretaceous deformation and uplift: A superplume-related event? |
title_full_unstemmed |
Circum-Pacific mid-Cretaceous deformation and uplift: A superplume-related event? |
title_sort |
circum-pacific mid-cretaceous deformation and uplift: a superplume-related event? |
publisher |
Geological Society of America |
publishDate |
1995 |
url |
http://nora.nerc.ac.uk/id/eprint/515878/ https://doi.org/10.1130/0091-7613(1995)023<0491:CPMCDA>2.3.CO;2 |
geographic |
Pacific West Antarctica |
geographic_facet |
Pacific West Antarctica |
genre |
Antarc* Antarctica West Antarctica Alaska |
genre_facet |
Antarc* Antarctica West Antarctica Alaska |
op_relation |
Vaughan, Alan P.M. 1995 Circum-Pacific mid-Cretaceous deformation and uplift: A superplume-related event? Geology, 23 (6). 491-494. https://doi.org/10.1130/0091-7613(1995)023<0491:CPMCDA>2.3.CO;2 <https://doi.org/10.1130/0091-7613(1995)023<0491:CPMCDA>2.3.CO;2> |
op_doi |
https://doi.org/10.1130/0091-7613(1995)023<0491:CPMCDA>2.3.CO;2 |
_version_ |
1766251631867854848 |