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

Bibliographic Details
Published in:Gondwana Research
Main Authors: Elliot, D.H., Fanning, Christopher
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier
Subjects:
Keywords: Antarctica
Beacon
geochronology
Permian-Triassic
Zircon
Shackleton
Transantarctic Mountains
Shackleton Glacier
Antarc*
Antarctica
Online Access:http://hdl.handle.net/1885/33708
https://doi.org/10.1016/j.gr.2007.05.003
https://openresearch-repository.anu.edu.au/bitstream/1885/33708/5/FanningCM_RSES_2008_01_Elliot.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/33708/7/01_Elliot_Detrital_zircons_from_upper_2008.pdf.jpg
Description
Summary: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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