Continental reworking during overprinting orogenic events, southern Prince Charles Mountains, east Antarctica

© The Author 2009. Published by Oxford University Press. All rights reserved. In situ electron microprobe monazite dating and mineral equilibria modelling of amphibolite-granulite-facies metapelites from the southern Prince Charles Mountains, East Antarctica has been carried out to unravel the P-T c...

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Published in:Journal of Petrology
Main Authors: Phillips, G., Kelsey, D., Corvino, A., Dutch, R.
Format: Article in Journal/Newspaper
Language:English
Published: Oxford Univ Press 2009
Subjects:
Online Access:http://hdl.handle.net/2440/56866
https://doi.org/10.1093/petrology/egp065
id ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/56866
record_format openpolar
spelling ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/56866 2023-12-24T10:11:30+01:00 Continental reworking during overprinting orogenic events, southern Prince Charles Mountains, east Antarctica Phillips, G. Kelsey, D. Corvino, A. Dutch, R. 2009 http://hdl.handle.net/2440/56866 https://doi.org/10.1093/petrology/egp065 en eng Oxford Univ Press http://purl.org/au-research/grants/arc/DP0665094 Journal of Petrology, 2009; 50(11):2017-2041 0022-3530 1460-2415 http://hdl.handle.net/2440/56866 doi:10.1093/petrology/egp065 http://dx.doi.org/10.1093/petrology/egp065 continental reworking mineral equilibria modelling monazite Prydz orogenic event Rayner orogenic event Journal article 2009 ftunivadelaidedl https://doi.org/10.1093/petrology/egp065 2023-11-27T23:26:06Z © The Author 2009. Published by Oxford University Press. All rights reserved. In situ electron microprobe monazite dating and mineral equilibria modelling of amphibolite-granulite-facies metapelites from the southern Prince Charles Mountains, East Antarctica has been carried out to unravel the P-T conditions, spatial extent and structural style of two overprinting orogenic records. This study shows that: (1) rocks of the northern Palaeoproterozoic Lambert Complex were pervasively reworked at peak conditions (6·5-7·1 kbar and 790-810°C) during the Early Neoproterozoic Rayner orogenic event; (2) rocks of the southern Lambert Complex experienced pervasive deformation and metamorphism at peak conditions (5·8-6·1 kbar and 625-635°C) during Early Palaeozoic Prydz orogenic activity; (3) in regions of the Lambert Complex reworked during the Rayner orogenic event, Prydz-aged orogenesis was highly localized. The distribution of orogenic activity pertaining to the Rayner and Prydz orogenic events in the southern Prince Charles Mountains can be attributed to (1) the development of a southward directed (current coordinates) orogenic front that propagated from an Early Neoproterozoic collision between India and Antarctica, and (2) rock fertility (i.e. availability of free fluid) during Early Palaeozoic intraplate orogenesis that was driven by far-field stresses generated by a collision of India-Antarctica with the Mawson Craton. © The Author 2009. Published by Oxford University Press. All rights reserved. G. Phillips, D. E. Kelsey, A. F. Corvino and R. A. Dutch Article in Journal/Newspaper Antarc* Antarctica East Antarctica Prince Charles Mountains The University of Adelaide: Digital Library East Antarctica Prince Charles Mountains ENVELOPE(67.246,67.246,-71.427,-71.427) Rayner ENVELOPE(-45.166,-45.166,-60.650,-60.650) Kelsey ENVELOPE(-22.306,-22.306,-80.448,-80.448) Journal of Petrology 50 11 2017 2041
institution Open Polar
collection The University of Adelaide: Digital Library
op_collection_id ftunivadelaidedl
language English
topic continental reworking
mineral equilibria modelling
monazite
Prydz orogenic event
Rayner orogenic event
spellingShingle continental reworking
mineral equilibria modelling
monazite
Prydz orogenic event
Rayner orogenic event
Phillips, G.
Kelsey, D.
Corvino, A.
Dutch, R.
Continental reworking during overprinting orogenic events, southern Prince Charles Mountains, east Antarctica
topic_facet continental reworking
mineral equilibria modelling
monazite
Prydz orogenic event
Rayner orogenic event
description © The Author 2009. Published by Oxford University Press. All rights reserved. In situ electron microprobe monazite dating and mineral equilibria modelling of amphibolite-granulite-facies metapelites from the southern Prince Charles Mountains, East Antarctica has been carried out to unravel the P-T conditions, spatial extent and structural style of two overprinting orogenic records. This study shows that: (1) rocks of the northern Palaeoproterozoic Lambert Complex were pervasively reworked at peak conditions (6·5-7·1 kbar and 790-810°C) during the Early Neoproterozoic Rayner orogenic event; (2) rocks of the southern Lambert Complex experienced pervasive deformation and metamorphism at peak conditions (5·8-6·1 kbar and 625-635°C) during Early Palaeozoic Prydz orogenic activity; (3) in regions of the Lambert Complex reworked during the Rayner orogenic event, Prydz-aged orogenesis was highly localized. The distribution of orogenic activity pertaining to the Rayner and Prydz orogenic events in the southern Prince Charles Mountains can be attributed to (1) the development of a southward directed (current coordinates) orogenic front that propagated from an Early Neoproterozoic collision between India and Antarctica, and (2) rock fertility (i.e. availability of free fluid) during Early Palaeozoic intraplate orogenesis that was driven by far-field stresses generated by a collision of India-Antarctica with the Mawson Craton. © The Author 2009. Published by Oxford University Press. All rights reserved. G. Phillips, D. E. Kelsey, A. F. Corvino and R. A. Dutch
format Article in Journal/Newspaper
author Phillips, G.
Kelsey, D.
Corvino, A.
Dutch, R.
author_facet Phillips, G.
Kelsey, D.
Corvino, A.
Dutch, R.
author_sort Phillips, G.
title Continental reworking during overprinting orogenic events, southern Prince Charles Mountains, east Antarctica
title_short Continental reworking during overprinting orogenic events, southern Prince Charles Mountains, east Antarctica
title_full Continental reworking during overprinting orogenic events, southern Prince Charles Mountains, east Antarctica
title_fullStr Continental reworking during overprinting orogenic events, southern Prince Charles Mountains, east Antarctica
title_full_unstemmed Continental reworking during overprinting orogenic events, southern Prince Charles Mountains, east Antarctica
title_sort continental reworking during overprinting orogenic events, southern prince charles mountains, east antarctica
publisher Oxford Univ Press
publishDate 2009
url http://hdl.handle.net/2440/56866
https://doi.org/10.1093/petrology/egp065
long_lat ENVELOPE(67.246,67.246,-71.427,-71.427)
ENVELOPE(-45.166,-45.166,-60.650,-60.650)
ENVELOPE(-22.306,-22.306,-80.448,-80.448)
geographic East Antarctica
Prince Charles Mountains
Rayner
Kelsey
geographic_facet East Antarctica
Prince Charles Mountains
Rayner
Kelsey
genre Antarc*
Antarctica
East Antarctica
Prince Charles Mountains
genre_facet Antarc*
Antarctica
East Antarctica
Prince Charles Mountains
op_source http://dx.doi.org/10.1093/petrology/egp065
op_relation http://purl.org/au-research/grants/arc/DP0665094
Journal of Petrology, 2009; 50(11):2017-2041
0022-3530
1460-2415
http://hdl.handle.net/2440/56866
doi:10.1093/petrology/egp065
op_doi https://doi.org/10.1093/petrology/egp065
container_title Journal of Petrology
container_volume 50
container_issue 11
container_start_page 2017
op_container_end_page 2041
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