Detrital zircons from upper Permian and lower Triassic Victoria Group sandstones, Shackleton Glacier region, Antarctica: Evidence for multiple sources along the Gondwana plate margin
In the central Transantarctic Mountains region, siliciclastic strata of the Permian-Triassic Victoria Group (Beacon Supergroup), the Gondwana sequence in Antarctica, have both cratonic and magmatic arc provenance. Volcaniclastic strata occur in the upper
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ftanucanberra:oai:digitalcollections.anu.edu.au:1885/33708 2023-05-15T13:57:36+02:00 Detrital zircons from upper Permian and lower Triassic Victoria Group sandstones, Shackleton Glacier region, Antarctica: Evidence for multiple sources along the Gondwana plate margin Elliot, D.H. Fanning, Christopher 2015-12-08T22:26:37Z http://hdl.handle.net/1885/33708 unknown Elsevier 1342-937X http://hdl.handle.net/1885/33708 Gondwana Research Keywords: Antarctica Beacon geochronology Permian-Triassic Zircon Journal article 2015 ftanucanberra 2015-12-28T23:24:20Z In the central Transantarctic Mountains region, siliciclastic strata of the Permian-Triassic Victoria Group (Beacon Supergroup), the Gondwana sequence in Antarctica, have both cratonic and magmatic arc provenance. Volcaniclastic strata occur in the upper Article in Journal/Newspaper Antarc* Antarctica Shackleton Glacier Australian National University: ANU Digital Collections Shackleton Shackleton Glacier ENVELOPE(-37.200,-37.200,-54.133,-54.133) Transantarctic Mountains |
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Open Polar |
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Australian National University: ANU Digital Collections |
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ftanucanberra |
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unknown |
topic |
Keywords: Antarctica Beacon geochronology Permian-Triassic Zircon |
spellingShingle |
Keywords: Antarctica Beacon geochronology Permian-Triassic Zircon Elliot, D.H. Fanning, Christopher Detrital zircons from upper Permian and lower Triassic Victoria Group sandstones, Shackleton Glacier region, Antarctica: Evidence for multiple sources along the Gondwana plate margin |
topic_facet |
Keywords: Antarctica Beacon geochronology Permian-Triassic Zircon |
description |
In the central Transantarctic Mountains region, siliciclastic strata of the Permian-Triassic Victoria Group (Beacon Supergroup), the Gondwana sequence in Antarctica, have both cratonic and magmatic arc provenance. Volcaniclastic strata occur in the upper |
format |
Article in Journal/Newspaper |
author |
Elliot, D.H. Fanning, Christopher |
author_facet |
Elliot, D.H. Fanning, Christopher |
author_sort |
Elliot, D.H. |
title |
Detrital zircons from upper Permian and lower Triassic Victoria Group sandstones, Shackleton Glacier region, Antarctica: Evidence for multiple sources along the Gondwana plate margin |
title_short |
Detrital zircons from upper Permian and lower Triassic Victoria Group sandstones, Shackleton Glacier region, Antarctica: Evidence for multiple sources along the Gondwana plate margin |
title_full |
Detrital zircons from upper Permian and lower Triassic Victoria Group sandstones, Shackleton Glacier region, Antarctica: Evidence for multiple sources along the Gondwana plate margin |
title_fullStr |
Detrital zircons from upper Permian and lower Triassic Victoria Group sandstones, Shackleton Glacier region, Antarctica: Evidence for multiple sources along the Gondwana plate margin |
title_full_unstemmed |
Detrital zircons from upper Permian and lower Triassic Victoria Group sandstones, Shackleton Glacier region, Antarctica: Evidence for multiple sources along the Gondwana plate margin |
title_sort |
detrital zircons from upper permian and lower triassic victoria group sandstones, shackleton glacier region, antarctica: evidence for multiple sources along the gondwana plate margin |
publisher |
Elsevier |
publishDate |
2015 |
url |
http://hdl.handle.net/1885/33708 |
long_lat |
ENVELOPE(-37.200,-37.200,-54.133,-54.133) |
geographic |
Shackleton Shackleton Glacier Transantarctic Mountains |
geographic_facet |
Shackleton Shackleton Glacier Transantarctic Mountains |
genre |
Antarc* Antarctica Shackleton Glacier |
genre_facet |
Antarc* Antarctica Shackleton Glacier |
op_source |
Gondwana Research |
op_relation |
1342-937X http://hdl.handle.net/1885/33708 |
_version_ |
1766265306360053760 |