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://eprints.utas.edu.au/45103/
https://eprints.utas.edu.au/45103/1/Daczko%2B%2BGondwanaAntarctica_SciRep_2018.pdf
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spelling ftunivtasmania:oai:eprints.utas.edu.au:45103 2023-05-15T13:41:50+02:00 A cryptic Gondwana-forming orogen located in Antarctica Daczko, NR Halpin, JA Fitzsimons, ICW Whittaker, JM 2018 application/pdf https://eprints.utas.edu.au/45103/ https://eprints.utas.edu.au/45103/1/Daczko%2B%2BGondwanaAntarctica_SciRep_2018.pdf en eng Nature Publishing Group https://eprints.utas.edu.au/45103/1/Daczko%2B%2BGondwanaAntarctica_SciRep_2018.pdf Daczko, NR, Halpin, JA orcid:0000-0002-4992-8681 , Fitzsimons, ICW and Whittaker, JM orcid:0000-0002-3170-3935 2018 , 'A cryptic Gondwana-forming orogen located in Antarctica' , Scientific Reports, vol. 8 , pp. 1-9 , doi:10.1038/s41598-018-26530-1 <http://dx.doi.org/10.1038/s41598-018-26530-1>. Antarctica plate reconstruction Gondwana Article PeerReviewed 2018 ftunivtasmania https://doi.org/10.1038/s41598-018-26530-1 2022-03-07T23:17:04Z 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 3000–5000 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 130°E, one of Indian affinity with dominant ca. 980–900 Ma ages (Indo-Antarctica) and one of Australian affinity with dominant ca. 1190–1140 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 ∼94°E. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica University of Tasmania: UTas ePrints Antarctic East Antarctica Indian Mirny ENVELOPE(93.009,93.009,-66.553,-66.553) Scientific Reports 8 1
institution Open Polar
collection University of Tasmania: UTas ePrints
op_collection_id ftunivtasmania
language English
topic Antarctica
plate reconstruction
Gondwana
spellingShingle Antarctica
plate reconstruction
Gondwana
Daczko, NR
Halpin, JA
Fitzsimons, ICW
Whittaker, JM
A cryptic Gondwana-forming orogen located in Antarctica
topic_facet Antarctica
plate reconstruction
Gondwana
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 3000–5000 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 130°E, one of Indian affinity with dominant ca. 980–900 Ma ages (Indo-Antarctica) and one of Australian affinity with dominant ca. 1190–1140 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 ∼94°E.
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://eprints.utas.edu.au/45103/
https://eprints.utas.edu.au/45103/1/Daczko%2B%2BGondwanaAntarctica_SciRep_2018.pdf
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 https://eprints.utas.edu.au/45103/1/Daczko%2B%2BGondwanaAntarctica_SciRep_2018.pdf
Daczko, NR, Halpin, JA orcid:0000-0002-4992-8681 , Fitzsimons, ICW and Whittaker, JM orcid:0000-0002-3170-3935 2018 , 'A cryptic Gondwana-forming orogen located in Antarctica' , Scientific Reports, vol. 8 , pp. 1-9 , doi:10.1038/s41598-018-26530-1 <http://dx.doi.org/10.1038/s41598-018-26530-1>.
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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