Jurassic silicic volcanism in the Transantarctic Mountains: Was it related to plate margin processes or to Ferrar magmatism?
Abstract Silicic volcanism in the Transantarctic Mountains, represented by rhyolitic tuff that mainly precedes emplacement of the Ferrar Large Igneous Province, is important in interpretation of the tectonic evolution of the Antarctic sector of Gondwana. Sr and Nd isotope data indicate that the tuff...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.517.6029 2023-05-15T13:40:47+02:00 Jurassic silicic volcanism in the Transantarctic Mountains: Was it related to plate margin processes or to Ferrar magmatism? The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.517.6029 http://pubs.usgs.gov/of/2007/1047/srp/srp051/of2007-1047srp051.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.517.6029 http://pubs.usgs.gov/of/2007/1047/srp/srp051/of2007-1047srp051.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.usgs.gov/of/2007/1047/srp/srp051/of2007-1047srp051.pdf text ftciteseerx 2016-01-08T09:56:33Z Abstract Silicic volcanism in the Transantarctic Mountains, represented by rhyolitic tuff that mainly precedes emplacement of the Ferrar Large Igneous Province, is important in interpretation of the tectonic evolution of the Antarctic sector of Gondwana. Sr and Nd isotope data indicate that the tuffs are not directly related to Ferrar magmatism nor to melting of the underlying Ross orogen crust yet zircon gives a U-Pb age of 182.7±1.8 Ma, similar to the U/Pb age for the Ferrar. Distribution of the silicic tuffs along 1400 km of the Transantarctic Mountains suggests, alternatively, a relationship to the Gondwana plate margin. Although West Antarctica comprises Mesoproterozoic crustal terrains, few analyzed rocks are compatible isotopically with the Lower Jurassic tuffs. The source of the tuffs must lie in unexposed Early Jurassic magmatic centers in West Antarctica or an unexposed crustal terrain beneath the Transantarctic Mountains. Text Antarc* Antarctic Antarctica West Antarctica Unknown Antarctic The Antarctic Transantarctic Mountains West Antarctica |
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English |
description |
Abstract Silicic volcanism in the Transantarctic Mountains, represented by rhyolitic tuff that mainly precedes emplacement of the Ferrar Large Igneous Province, is important in interpretation of the tectonic evolution of the Antarctic sector of Gondwana. Sr and Nd isotope data indicate that the tuffs are not directly related to Ferrar magmatism nor to melting of the underlying Ross orogen crust yet zircon gives a U-Pb age of 182.7±1.8 Ma, similar to the U/Pb age for the Ferrar. Distribution of the silicic tuffs along 1400 km of the Transantarctic Mountains suggests, alternatively, a relationship to the Gondwana plate margin. Although West Antarctica comprises Mesoproterozoic crustal terrains, few analyzed rocks are compatible isotopically with the Lower Jurassic tuffs. The source of the tuffs must lie in unexposed Early Jurassic magmatic centers in West Antarctica or an unexposed crustal terrain beneath the Transantarctic Mountains. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
title |
Jurassic silicic volcanism in the Transantarctic Mountains: Was it related to plate margin processes or to Ferrar magmatism? |
spellingShingle |
Jurassic silicic volcanism in the Transantarctic Mountains: Was it related to plate margin processes or to Ferrar magmatism? |
title_short |
Jurassic silicic volcanism in the Transantarctic Mountains: Was it related to plate margin processes or to Ferrar magmatism? |
title_full |
Jurassic silicic volcanism in the Transantarctic Mountains: Was it related to plate margin processes or to Ferrar magmatism? |
title_fullStr |
Jurassic silicic volcanism in the Transantarctic Mountains: Was it related to plate margin processes or to Ferrar magmatism? |
title_full_unstemmed |
Jurassic silicic volcanism in the Transantarctic Mountains: Was it related to plate margin processes or to Ferrar magmatism? |
title_sort |
jurassic silicic volcanism in the transantarctic mountains: was it related to plate margin processes or to ferrar magmatism? |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.517.6029 http://pubs.usgs.gov/of/2007/1047/srp/srp051/of2007-1047srp051.pdf |
geographic |
Antarctic The Antarctic Transantarctic Mountains West Antarctica |
geographic_facet |
Antarctic The Antarctic Transantarctic Mountains West Antarctica |
genre |
Antarc* Antarctic Antarctica West Antarctica |
genre_facet |
Antarc* Antarctic Antarctica West Antarctica |
op_source |
http://pubs.usgs.gov/of/2007/1047/srp/srp051/of2007-1047srp051.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.517.6029 http://pubs.usgs.gov/of/2007/1047/srp/srp051/of2007-1047srp051.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766139966056824832 |