The structural and metamorphic geology of basement rocks in the mcmurdo sound area, antarctica

The petrography and structure of three small areas, the Nussbaum Riegel and the north and south sides of the Garwood Valley in the "Dry Valleys" region of Victoria Land, Antarctica, are described and discussed. The rocks are mostly pure or impure marbles plus lesser quantities of amphiboli...

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Published in:Journal of the Geological Society of Australia
Main Authors: Williams, P. F., Hobbs, B. E., Vernon, R. H., Anderson, D. E.
Format: Article in Journal/Newspaper
Language:English
Published: 1971
Subjects:
Online Access:https://researchers.mq.edu.au/en/publications/ebbaeb17-eb5f-4753-afb9-b2091313370d
https://doi.org/10.1080/00167617108728751
http://www.scopus.com/inward/record.url?scp=0000015422&partnerID=8YFLogxK
id ftmacquarieunicr:oai:https://researchers.mq.edu.au:publications/ebbaeb17-eb5f-4753-afb9-b2091313370d
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spelling ftmacquarieunicr:oai:https://researchers.mq.edu.au:publications/ebbaeb17-eb5f-4753-afb9-b2091313370d 2023-05-15T13:51:16+02:00 The structural and metamorphic geology of basement rocks in the mcmurdo sound area, antarctica Williams, P. F. Hobbs, B. E. Vernon, R. H. Anderson, D. E. 1971 https://researchers.mq.edu.au/en/publications/ebbaeb17-eb5f-4753-afb9-b2091313370d https://doi.org/10.1080/00167617108728751 http://www.scopus.com/inward/record.url?scp=0000015422&partnerID=8YFLogxK eng eng info:eu-repo/semantics/restrictedAccess Williams , P F , Hobbs , B E , Vernon , R H & Anderson , D E 1971 , ' The structural and metamorphic geology of basement rocks in the mcmurdo sound area, antarctica ' , Journal of the Geological Society of Australia , vol. 18 , no. 2 , pp. 127-142 . https://doi.org/10.1080/00167617108728751 article 1971 ftmacquarieunicr https://doi.org/10.1080/00167617108728751 2022-02-18T14:38:28Z The petrography and structure of three small areas, the Nussbaum Riegel and the north and south sides of the Garwood Valley in the "Dry Valleys" region of Victoria Land, Antarctica, are described and discussed. The rocks are mostly pure or impure marbles plus lesser quantities of amphibolite, schist and quartz-feldspar rocks, and mineral assemblages indicate that they have been metamorphosed under conditions of the amphibolite fades, and possibly, locally under conditions transitional to the granulite facies. In general they have not suffered retrograde metamorphism. Nussbaum Riegel is characterized by isoclinal folds and very well-developed boudinage structure. Examination of the boudins reveals that the competent beds behaved in a ductile manner when failing parallel to the fold axis and in a brittle manner when failing perpendicular to the fold axis. An explanation for this observation is offered, based on variation in strain rate in various directions during the development of the fold. The Garwood Valley areas are complex and two generations of folds are recognized. The large scale structure of the south side of the Garwood Valley is interpreted as a tight basin resulting from the interference of the two generations of folds. The large scale structure of the north side of the Garwood Valley is believed to be similar in style to that of the south side, but insufficient data are obtainable to allow detailed interpretation. Copyright. Article in Journal/Newspaper Antarc* Antarctica Antarctica Journal McMurdo Sound Victoria Land Macquarie University Research Portal Victoria Land McMurdo Sound Garwood ENVELOPE(164.283,164.283,-78.033,-78.033) Garwood Valley ENVELOPE(164.167,164.167,-78.033,-78.033) Nussbaum Riegel ENVELOPE(162.767,162.767,-77.667,-77.667) Journal of the Geological Society of Australia 18 2 127 142
institution Open Polar
collection Macquarie University Research Portal
op_collection_id ftmacquarieunicr
language English
description The petrography and structure of three small areas, the Nussbaum Riegel and the north and south sides of the Garwood Valley in the "Dry Valleys" region of Victoria Land, Antarctica, are described and discussed. The rocks are mostly pure or impure marbles plus lesser quantities of amphibolite, schist and quartz-feldspar rocks, and mineral assemblages indicate that they have been metamorphosed under conditions of the amphibolite fades, and possibly, locally under conditions transitional to the granulite facies. In general they have not suffered retrograde metamorphism. Nussbaum Riegel is characterized by isoclinal folds and very well-developed boudinage structure. Examination of the boudins reveals that the competent beds behaved in a ductile manner when failing parallel to the fold axis and in a brittle manner when failing perpendicular to the fold axis. An explanation for this observation is offered, based on variation in strain rate in various directions during the development of the fold. The Garwood Valley areas are complex and two generations of folds are recognized. The large scale structure of the south side of the Garwood Valley is interpreted as a tight basin resulting from the interference of the two generations of folds. The large scale structure of the north side of the Garwood Valley is believed to be similar in style to that of the south side, but insufficient data are obtainable to allow detailed interpretation. Copyright.
format Article in Journal/Newspaper
author Williams, P. F.
Hobbs, B. E.
Vernon, R. H.
Anderson, D. E.
spellingShingle Williams, P. F.
Hobbs, B. E.
Vernon, R. H.
Anderson, D. E.
The structural and metamorphic geology of basement rocks in the mcmurdo sound area, antarctica
author_facet Williams, P. F.
Hobbs, B. E.
Vernon, R. H.
Anderson, D. E.
author_sort Williams, P. F.
title The structural and metamorphic geology of basement rocks in the mcmurdo sound area, antarctica
title_short The structural and metamorphic geology of basement rocks in the mcmurdo sound area, antarctica
title_full The structural and metamorphic geology of basement rocks in the mcmurdo sound area, antarctica
title_fullStr The structural and metamorphic geology of basement rocks in the mcmurdo sound area, antarctica
title_full_unstemmed The structural and metamorphic geology of basement rocks in the mcmurdo sound area, antarctica
title_sort structural and metamorphic geology of basement rocks in the mcmurdo sound area, antarctica
publishDate 1971
url https://researchers.mq.edu.au/en/publications/ebbaeb17-eb5f-4753-afb9-b2091313370d
https://doi.org/10.1080/00167617108728751
http://www.scopus.com/inward/record.url?scp=0000015422&partnerID=8YFLogxK
long_lat ENVELOPE(164.283,164.283,-78.033,-78.033)
ENVELOPE(164.167,164.167,-78.033,-78.033)
ENVELOPE(162.767,162.767,-77.667,-77.667)
geographic Victoria Land
McMurdo Sound
Garwood
Garwood Valley
Nussbaum Riegel
geographic_facet Victoria Land
McMurdo Sound
Garwood
Garwood Valley
Nussbaum Riegel
genre Antarc*
Antarctica
Antarctica Journal
McMurdo Sound
Victoria Land
genre_facet Antarc*
Antarctica
Antarctica Journal
McMurdo Sound
Victoria Land
op_source Williams , P F , Hobbs , B E , Vernon , R H & Anderson , D E 1971 , ' The structural and metamorphic geology of basement rocks in the mcmurdo sound area, antarctica ' , Journal of the Geological Society of Australia , vol. 18 , no. 2 , pp. 127-142 . https://doi.org/10.1080/00167617108728751
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1080/00167617108728751
container_title Journal of the Geological Society of Australia
container_volume 18
container_issue 2
container_start_page 127
op_container_end_page 142
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