Revisiting the Australian-Antarctic ocean-continent transition zone using petrological and geophysical characterization of exhumed subcontinental mantle
The final lithospheric breakup of the Australian‐Antarctic rift system remains controversial due to sparse geological constraints on the nature of the basement along the ocean‐continent transition (OCT) zones. We present new interpretations of multichannel seismic reflection transects and new petrol...
Published in: | Geochemistry, Geophysics, Geosystems |
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Amer Geophysical Union
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Online Access: | https://doi.org/10.1029/2020GC009040 http://ecite.utas.edu.au/139766 |
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ftunivtasecite:oai:ecite.utas.edu.au:139766 2023-05-15T13:42:40+02:00 Revisiting the Australian-Antarctic ocean-continent transition zone using petrological and geophysical characterization of exhumed subcontinental mantle McCarthy, A Falloon, TJ Sauermilch, I Whittaker, JM Niida, K Green, DH 2020 application/pdf https://doi.org/10.1029/2020GC009040 http://ecite.utas.edu.au/139766 en eng Amer Geophysical Union http://ecite.utas.edu.au/139766/1/139766 - Revisiting the Australian‐Antarctic ocean‐continent transition zone using petrological and geophysical characterization of exhumed subcontinental mantle.pdf http://dx.doi.org/10.1029/2020GC009040 McCarthy, A and Falloon, TJ and Sauermilch, I and Whittaker, JM and Niida, K and Green, DH, Revisiting the Australian-Antarctic ocean-continent transition zone using petrological and geophysical characterization of exhumed subcontinental mantle, Geochemistry Geophysics Geosystems, 21, (7) Article e2020GC009040. ISSN 1525-2027 (2020) [Refereed Article] http://ecite.utas.edu.au/139766 Earth Sciences Geology Igneous and metamorphic petrology Refereed Article PeerReviewed 2020 ftunivtasecite https://doi.org/10.1029/2020GC009040 2022-08-29T22:18:01Z The final lithospheric breakup of the Australian‐Antarctic rift system remains controversial due to sparse geological constraints on the nature of the basement along the ocean‐continent transition (OCT) zones. We present new interpretations of multichannel seismic reflection transects and new petrological data of dredged mantle rocks along the East Antarctic margin (Seamount B, offshore Terre Adlie). By combining both data sets, we show that a 50100 km wide domain of cold and fertile subcontinental mantle was exhumed along the magma‐poor Antarctic margin. This study represents only the second locality, along with the Iberia‐Newfoundland margins, where the importance of exhumed mantle domains along OCTs can be clearly identified. The dredged peridotites preserve characteristics similar to mantle xenoliths found in syn‐ to post‐rift volcanism at the eastern end of the Australian margin (Victoria and Tasmania), indicating the exhumation of fertile subcontinental mantle during rifting between Australia and Antarctica. Seamount B represents the initial stages of exhumation of cold subcontinental lithosphere along an OCT during rifting. This thick mantle domain was likely affected by melt impregnation at high pressure (8 kbar), leading to the formation of plagioclase‐pyroxenites. The combination of continental rifted blocks, a wide domain of volcanic‐poor subcontinental mantle and (ultra‐) slow spreading is analogous to OCTs from the Jurassic Western Tethys and Iberia‐Newfoundland rifted margins. Additionally, evidence of melt stagnation at high pressure suggests that magmatism along the Australian‐Antarctic rifted margins was sufficient to form magnetic anomalies that can be used as isochrons despite their formation in lithosphere other than mature, steady‐state ocean crust. Article in Journal/Newspaper Antarc* Antarctic Antarctic Ocean Antarctica Newfoundland eCite UTAS (University of Tasmania) Antarctic Antarctic Ocean Geochemistry, Geophysics, Geosystems 21 7 |
institution |
Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Geology Igneous and metamorphic petrology |
spellingShingle |
Earth Sciences Geology Igneous and metamorphic petrology McCarthy, A Falloon, TJ Sauermilch, I Whittaker, JM Niida, K Green, DH Revisiting the Australian-Antarctic ocean-continent transition zone using petrological and geophysical characterization of exhumed subcontinental mantle |
topic_facet |
Earth Sciences Geology Igneous and metamorphic petrology |
description |
The final lithospheric breakup of the Australian‐Antarctic rift system remains controversial due to sparse geological constraints on the nature of the basement along the ocean‐continent transition (OCT) zones. We present new interpretations of multichannel seismic reflection transects and new petrological data of dredged mantle rocks along the East Antarctic margin (Seamount B, offshore Terre Adlie). By combining both data sets, we show that a 50100 km wide domain of cold and fertile subcontinental mantle was exhumed along the magma‐poor Antarctic margin. This study represents only the second locality, along with the Iberia‐Newfoundland margins, where the importance of exhumed mantle domains along OCTs can be clearly identified. The dredged peridotites preserve characteristics similar to mantle xenoliths found in syn‐ to post‐rift volcanism at the eastern end of the Australian margin (Victoria and Tasmania), indicating the exhumation of fertile subcontinental mantle during rifting between Australia and Antarctica. Seamount B represents the initial stages of exhumation of cold subcontinental lithosphere along an OCT during rifting. This thick mantle domain was likely affected by melt impregnation at high pressure (8 kbar), leading to the formation of plagioclase‐pyroxenites. The combination of continental rifted blocks, a wide domain of volcanic‐poor subcontinental mantle and (ultra‐) slow spreading is analogous to OCTs from the Jurassic Western Tethys and Iberia‐Newfoundland rifted margins. Additionally, evidence of melt stagnation at high pressure suggests that magmatism along the Australian‐Antarctic rifted margins was sufficient to form magnetic anomalies that can be used as isochrons despite their formation in lithosphere other than mature, steady‐state ocean crust. |
format |
Article in Journal/Newspaper |
author |
McCarthy, A Falloon, TJ Sauermilch, I Whittaker, JM Niida, K Green, DH |
author_facet |
McCarthy, A Falloon, TJ Sauermilch, I Whittaker, JM Niida, K Green, DH |
author_sort |
McCarthy, A |
title |
Revisiting the Australian-Antarctic ocean-continent transition zone using petrological and geophysical characterization of exhumed subcontinental mantle |
title_short |
Revisiting the Australian-Antarctic ocean-continent transition zone using petrological and geophysical characterization of exhumed subcontinental mantle |
title_full |
Revisiting the Australian-Antarctic ocean-continent transition zone using petrological and geophysical characterization of exhumed subcontinental mantle |
title_fullStr |
Revisiting the Australian-Antarctic ocean-continent transition zone using petrological and geophysical characterization of exhumed subcontinental mantle |
title_full_unstemmed |
Revisiting the Australian-Antarctic ocean-continent transition zone using petrological and geophysical characterization of exhumed subcontinental mantle |
title_sort |
revisiting the australian-antarctic ocean-continent transition zone using petrological and geophysical characterization of exhumed subcontinental mantle |
publisher |
Amer Geophysical Union |
publishDate |
2020 |
url |
https://doi.org/10.1029/2020GC009040 http://ecite.utas.edu.au/139766 |
geographic |
Antarctic Antarctic Ocean |
geographic_facet |
Antarctic Antarctic Ocean |
genre |
Antarc* Antarctic Antarctic Ocean Antarctica Newfoundland |
genre_facet |
Antarc* Antarctic Antarctic Ocean Antarctica Newfoundland |
op_relation |
http://ecite.utas.edu.au/139766/1/139766 - Revisiting the Australian‐Antarctic ocean‐continent transition zone using petrological and geophysical characterization of exhumed subcontinental mantle.pdf http://dx.doi.org/10.1029/2020GC009040 McCarthy, A and Falloon, TJ and Sauermilch, I and Whittaker, JM and Niida, K and Green, DH, Revisiting the Australian-Antarctic ocean-continent transition zone using petrological and geophysical characterization of exhumed subcontinental mantle, Geochemistry Geophysics Geosystems, 21, (7) Article e2020GC009040. ISSN 1525-2027 (2020) [Refereed Article] http://ecite.utas.edu.au/139766 |
op_doi |
https://doi.org/10.1029/2020GC009040 |
container_title |
Geochemistry, Geophysics, Geosystems |
container_volume |
21 |
container_issue |
7 |
_version_ |
1766171150260371456 |