A cryptic Gondwana-forming orogen located in Antarctica

The most poorly exposed and least understood Gondwana-forming orogen lies largely hidden beneath ice in East Antarctica. Called the Kuunga orogen, its interpolation between scattered outcrops is speculative with differing and often contradictory trends proposed, and no consensus on the location of a...

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Published in:Scientific Reports
Main Authors: Daczko, NR, Halpin, JA, Fitzsimons, ICW, Whittaker, JM
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group 2018
Subjects:
Online Access:https://doi.org/10.1038/s41598-018-26530-1
http://www.ncbi.nlm.nih.gov/pubmed/29849064
http://ecite.utas.edu.au/126730
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spelling ftunivtasecite:oai:ecite.utas.edu.au:126730 2023-05-15T13:55:18+02:00 A cryptic Gondwana-forming orogen located in Antarctica Daczko, NR Halpin, JA Fitzsimons, ICW Whittaker, JM 2018 application/pdf https://doi.org/10.1038/s41598-018-26530-1 http://www.ncbi.nlm.nih.gov/pubmed/29849064 http://ecite.utas.edu.au/126730 en eng Nature Publishing Group http://ecite.utas.edu.au/126730/1/Daczko++GondwanaAntarctica_SciRep_2018.pdf http://dx.doi.org/10.1038/s41598-018-26530-1 Daczko, NR and Halpin, JA and Fitzsimons, ICW and Whittaker, JM, A cryptic Gondwana-forming orogen located in Antarctica, Scientific Reports, 8 Article 8371. ISSN 2045-2322 (2018) [Refereed Article] http://www.ncbi.nlm.nih.gov/pubmed/29849064 http://ecite.utas.edu.au/126730 Earth Sciences Geology Tectonics Refereed Article PeerReviewed 2018 ftunivtasecite https://doi.org/10.1038/s41598-018-26530-1 2019-12-13T22:25:09Z The most poorly exposed and least understood Gondwana-forming orogen lies largely hidden beneath ice in East Antarctica. Called the Kuunga orogen, its interpolation between scattered outcrops is speculative with differing and often contradictory trends proposed, and no consensus on the location of any sutures. While some discount a suture altogether, paleomagnetic data from Indo-Antarctica and Australo-Antarctica do require 30005000 km relative displacement during Ediacaran-Cambrian Gondwana amalgamation, suggesting that the Kuunga orogen sutured provinces of broadly Indian versus Australian affinity. Here we use compiled data from detrital zircons offshore of East Antarctica that fingerprint two coastal subglacial basement provinces between 60 and 130E, one of Indian affinity with dominant ca. 980900 Ma ages (Indo-Antarctica) and one of Australian affinity with dominant ca. 11901140 and ca. 1560 Ma ages (Australo-Antarctica). We combine this offshore compilation with existing and new onshore U-Pb geochronology and previous geophysical interpretations to delimit the Indo-Australo-Antarctic boundary at a prominent geophysical lineament which intersects the coast east of Mirny at ∼94E. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica eCite UTAS (University of Tasmania) Antarctic East Antarctica Indian Mirny ENVELOPE(93.009,93.009,-66.553,-66.553) Scientific Reports 8 1
institution Open Polar
collection eCite UTAS (University of Tasmania)
op_collection_id ftunivtasecite
language English
topic Earth Sciences
Geology
Tectonics
spellingShingle Earth Sciences
Geology
Tectonics
Daczko, NR
Halpin, JA
Fitzsimons, ICW
Whittaker, JM
A cryptic Gondwana-forming orogen located in Antarctica
topic_facet Earth Sciences
Geology
Tectonics
description The most poorly exposed and least understood Gondwana-forming orogen lies largely hidden beneath ice in East Antarctica. Called the Kuunga orogen, its interpolation between scattered outcrops is speculative with differing and often contradictory trends proposed, and no consensus on the location of any sutures. While some discount a suture altogether, paleomagnetic data from Indo-Antarctica and Australo-Antarctica do require 30005000 km relative displacement during Ediacaran-Cambrian Gondwana amalgamation, suggesting that the Kuunga orogen sutured provinces of broadly Indian versus Australian affinity. Here we use compiled data from detrital zircons offshore of East Antarctica that fingerprint two coastal subglacial basement provinces between 60 and 130E, one of Indian affinity with dominant ca. 980900 Ma ages (Indo-Antarctica) and one of Australian affinity with dominant ca. 11901140 and ca. 1560 Ma ages (Australo-Antarctica). We combine this offshore compilation with existing and new onshore U-Pb geochronology and previous geophysical interpretations to delimit the Indo-Australo-Antarctic boundary at a prominent geophysical lineament which intersects the coast east of Mirny at ∼94E.
format Article in Journal/Newspaper
author Daczko, NR
Halpin, JA
Fitzsimons, ICW
Whittaker, JM
author_facet Daczko, NR
Halpin, JA
Fitzsimons, ICW
Whittaker, JM
author_sort Daczko, NR
title A cryptic Gondwana-forming orogen located in Antarctica
title_short A cryptic Gondwana-forming orogen located in Antarctica
title_full A cryptic Gondwana-forming orogen located in Antarctica
title_fullStr A cryptic Gondwana-forming orogen located in Antarctica
title_full_unstemmed A cryptic Gondwana-forming orogen located in Antarctica
title_sort cryptic gondwana-forming orogen located in antarctica
publisher Nature Publishing Group
publishDate 2018
url https://doi.org/10.1038/s41598-018-26530-1
http://www.ncbi.nlm.nih.gov/pubmed/29849064
http://ecite.utas.edu.au/126730
long_lat ENVELOPE(93.009,93.009,-66.553,-66.553)
geographic Antarctic
East Antarctica
Indian
Mirny
geographic_facet Antarctic
East Antarctica
Indian
Mirny
genre Antarc*
Antarctic
Antarctica
East Antarctica
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
op_relation http://ecite.utas.edu.au/126730/1/Daczko++GondwanaAntarctica_SciRep_2018.pdf
http://dx.doi.org/10.1038/s41598-018-26530-1
Daczko, NR and Halpin, JA and Fitzsimons, ICW and Whittaker, JM, A cryptic Gondwana-forming orogen located in Antarctica, Scientific Reports, 8 Article 8371. ISSN 2045-2322 (2018) [Refereed Article]
http://www.ncbi.nlm.nih.gov/pubmed/29849064
http://ecite.utas.edu.au/126730
op_doi https://doi.org/10.1038/s41598-018-26530-1
container_title Scientific Reports
container_volume 8
container_issue 1
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