Anatexis and crustal differentiation: Insights from the Fosdick migmatite-granite complex, West Antarctica ...
In the Fosdick migmatite-granite complex of West Antarctica, U-Pb geochronology of monazite in migmatites and zircon in granites records two episodes of high-temperature metamorphism, one in the Devonian-Carboniferous and another in the Cretaceous. For the older lower-grade event, whole-rock and zir...
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Online Access: | https://dx.doi.org/10.13016/m2501k http://hdl.handle.net/1903/15755 |
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ftdatacite:10.13016/m2501k 2023-08-27T04:04:45+02:00 Anatexis and crustal differentiation: Insights from the Fosdick migmatite-granite complex, West Antarctica ... Yakymchuk, Christopher 2014 https://dx.doi.org/10.13016/m2501k http://hdl.handle.net/1903/15755 en eng Digital Repository at the University of Maryland Geology FOS Earth and related environmental sciences Petrology Geochemistry geochronology granite isotope migmatite partial melting phase equilibria modeling Thesis thesis Dissertation Collection 2014 ftdatacite https://doi.org/10.13016/m2501k 2023-08-07T14:24:23Z In the Fosdick migmatite-granite complex of West Antarctica, U-Pb geochronology of monazite in migmatites and zircon in granites records two episodes of high-temperature metamorphism, one in the Devonian-Carboniferous and another in the Cretaceous. For the older lower-grade event, whole-rock and zircon isotope geochemistry of granites within the Fosdick complex are interpreted to record crustal reworking during metamorphism associated with continental arc magmatism along the East Gondwana convergent plate margin. By contrast, the geochemistry of correlative granites suites from along and across the same margin indicates a greater proportion of crustal growth. This suggests prominent arc-parallel and arc-normal variations in the mechanisms of crustal reworking versus growth in continental arc systems. Based on garnet Lu-Hf ages, the timing of peak metamorphism in the younger higher-grade event has been determined as c. 116-111 Ma. U-Pb ages of monazite from migmatites and zircon from anatectic granites ... Doctoral or Postdoctoral Thesis Antarc* Antarctica West Antarctica DataCite Metadata Store (German National Library of Science and Technology) West Antarctica |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Geology FOS Earth and related environmental sciences Petrology Geochemistry geochronology granite isotope migmatite partial melting phase equilibria modeling |
spellingShingle |
Geology FOS Earth and related environmental sciences Petrology Geochemistry geochronology granite isotope migmatite partial melting phase equilibria modeling Yakymchuk, Christopher Anatexis and crustal differentiation: Insights from the Fosdick migmatite-granite complex, West Antarctica ... |
topic_facet |
Geology FOS Earth and related environmental sciences Petrology Geochemistry geochronology granite isotope migmatite partial melting phase equilibria modeling |
description |
In the Fosdick migmatite-granite complex of West Antarctica, U-Pb geochronology of monazite in migmatites and zircon in granites records two episodes of high-temperature metamorphism, one in the Devonian-Carboniferous and another in the Cretaceous. For the older lower-grade event, whole-rock and zircon isotope geochemistry of granites within the Fosdick complex are interpreted to record crustal reworking during metamorphism associated with continental arc magmatism along the East Gondwana convergent plate margin. By contrast, the geochemistry of correlative granites suites from along and across the same margin indicates a greater proportion of crustal growth. This suggests prominent arc-parallel and arc-normal variations in the mechanisms of crustal reworking versus growth in continental arc systems. Based on garnet Lu-Hf ages, the timing of peak metamorphism in the younger higher-grade event has been determined as c. 116-111 Ma. U-Pb ages of monazite from migmatites and zircon from anatectic granites ... |
format |
Doctoral or Postdoctoral Thesis |
author |
Yakymchuk, Christopher |
author_facet |
Yakymchuk, Christopher |
author_sort |
Yakymchuk, Christopher |
title |
Anatexis and crustal differentiation: Insights from the Fosdick migmatite-granite complex, West Antarctica ... |
title_short |
Anatexis and crustal differentiation: Insights from the Fosdick migmatite-granite complex, West Antarctica ... |
title_full |
Anatexis and crustal differentiation: Insights from the Fosdick migmatite-granite complex, West Antarctica ... |
title_fullStr |
Anatexis and crustal differentiation: Insights from the Fosdick migmatite-granite complex, West Antarctica ... |
title_full_unstemmed |
Anatexis and crustal differentiation: Insights from the Fosdick migmatite-granite complex, West Antarctica ... |
title_sort |
anatexis and crustal differentiation: insights from the fosdick migmatite-granite complex, west antarctica ... |
publisher |
Digital Repository at the University of Maryland |
publishDate |
2014 |
url |
https://dx.doi.org/10.13016/m2501k http://hdl.handle.net/1903/15755 |
geographic |
West Antarctica |
geographic_facet |
West Antarctica |
genre |
Antarc* Antarctica West Antarctica |
genre_facet |
Antarc* Antarctica West Antarctica |
op_doi |
https://doi.org/10.13016/m2501k |
_version_ |
1775353319760330752 |