The tectonic evolution of Antarctica
Five tectonic provinces; three volcanic provinces (each characteristic of a particular set of tectonic conditions) and a Precambrian shield, are outlined and described, in an attempt to illustrate the tectonic evolution of Antarctica. Evidence is presented for at least three structural stages in the...
Main Author: | |
---|---|
Format: | Master Thesis |
Language: | English |
Published: |
University of Cambridge
1977
|
Subjects: | |
Online Access: | https://www.repository.cam.ac.uk/handle/1810/295127 https://doi.org/10.17863/CAM.42197 |
id |
ftunivcam:oai:www.repository.cam.ac.uk:1810/295127 |
---|---|
record_format |
openpolar |
spelling |
ftunivcam:oai:www.repository.cam.ac.uk:1810/295127 2024-01-21T10:00:37+01:00 The tectonic evolution of Antarctica Hamer, Richard Daniel 1977-05-01 application/pdf https://www.repository.cam.ac.uk/handle/1810/295127 https://doi.org/10.17863/CAM.42197 eng eng University of Cambridge Scott Polar Research Institute https://www.repository.cam.ac.uk/handle/1810/295127 doi:10.17863/CAM.42197 All Rights Reserved https://www.rioxx.net/licenses/all-rights-reserved/ Thesis Masters Master of Philosophy (MPhil) 1977 ftunivcam https://doi.org/10.17863/CAM.42197 2023-12-28T23:21:14Z Five tectonic provinces; three volcanic provinces (each characteristic of a particular set of tectonic conditions) and a Precambrian shield, are outlined and described, in an attempt to illustrate the tectonic evolution of Antarctica. Evidence is presented for at least three structural stages in the development of the Precambrian shield, though it is not as yet possible to delineate individual tectonic provinces within the shield area. From the late Proterozoic until the early Mesozoic, a series of tectonic provinces were successively stabilised and accreted onto the Pacific margin of the Precambrian shield. In the Mesozoic however, this unstable margin broke up into a number of blocks, as a result of differential movements between East and west Antarctica, associated with the fragmentation of Gondwanaland. Block tectonics, rifting and the development of faultbounded marginal basins, were accompanied by alkali volcanism in the late Cenozoic. This activity continues at the present. The proposed scheme is also viewed in the wider context of Gondwanaland and plate tectonics. Although the justification for long distance correlation of individual tectonic regions is called into question, four stages are illustrated in the evolution of the present Southern Hemisphere. Master Thesis Antarc* Antarctica West Antarctica Apollo - University of Cambridge Repository West Antarctica Pacific |
institution |
Open Polar |
collection |
Apollo - University of Cambridge Repository |
op_collection_id |
ftunivcam |
language |
English |
description |
Five tectonic provinces; three volcanic provinces (each characteristic of a particular set of tectonic conditions) and a Precambrian shield, are outlined and described, in an attempt to illustrate the tectonic evolution of Antarctica. Evidence is presented for at least three structural stages in the development of the Precambrian shield, though it is not as yet possible to delineate individual tectonic provinces within the shield area. From the late Proterozoic until the early Mesozoic, a series of tectonic provinces were successively stabilised and accreted onto the Pacific margin of the Precambrian shield. In the Mesozoic however, this unstable margin broke up into a number of blocks, as a result of differential movements between East and west Antarctica, associated with the fragmentation of Gondwanaland. Block tectonics, rifting and the development of faultbounded marginal basins, were accompanied by alkali volcanism in the late Cenozoic. This activity continues at the present. The proposed scheme is also viewed in the wider context of Gondwanaland and plate tectonics. Although the justification for long distance correlation of individual tectonic regions is called into question, four stages are illustrated in the evolution of the present Southern Hemisphere. |
format |
Master Thesis |
author |
Hamer, Richard Daniel |
spellingShingle |
Hamer, Richard Daniel The tectonic evolution of Antarctica |
author_facet |
Hamer, Richard Daniel |
author_sort |
Hamer, Richard Daniel |
title |
The tectonic evolution of Antarctica |
title_short |
The tectonic evolution of Antarctica |
title_full |
The tectonic evolution of Antarctica |
title_fullStr |
The tectonic evolution of Antarctica |
title_full_unstemmed |
The tectonic evolution of Antarctica |
title_sort |
tectonic evolution of antarctica |
publisher |
University of Cambridge |
publishDate |
1977 |
url |
https://www.repository.cam.ac.uk/handle/1810/295127 https://doi.org/10.17863/CAM.42197 |
geographic |
West Antarctica Pacific |
geographic_facet |
West Antarctica Pacific |
genre |
Antarc* Antarctica West Antarctica |
genre_facet |
Antarc* Antarctica West Antarctica |
op_relation |
https://www.repository.cam.ac.uk/handle/1810/295127 doi:10.17863/CAM.42197 |
op_rights |
All Rights Reserved https://www.rioxx.net/licenses/all-rights-reserved/ |
op_doi |
https://doi.org/10.17863/CAM.42197 |
_version_ |
1788703361582759936 |