INTERPRETATIONS OF COMPLICATED FOLDED STRUCTURES AT THE LOWER PARTS OF ANTARCTIC AND GREENLAND ICE SHEETS
Complicated folded structures were recently recorded by radar survey in the lower portions of the Antarctic and Greenland ice sheets. From a geological point of view the Antarctic and Greenland ice sheets are considered as geological features, while the ice is classified as sedimentary or metamorphi...
Published in: | GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Lomonosov Moscow State University
2015
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Online Access: | https://doi.org/10.24057/2071-9388-2015-8-1-4-15 https://doaj.org/article/b98cf9b177a24b2f961b6b50bd29b044 |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:b98cf9b177a24b2f961b6b50bd29b044 2023-05-15T13:59:44+02:00 INTERPRETATIONS OF COMPLICATED FOLDED STRUCTURES AT THE LOWER PARTS OF ANTARCTIC AND GREENLAND ICE SHEETS Alexey N. Markov Pavel G. Тalalay Dorthe Dahl-Jensen 2015-03-01 https://doi.org/10.24057/2071-9388-2015-8-1-4-15 https://doaj.org/article/b98cf9b177a24b2f961b6b50bd29b044 en eng Lomonosov Moscow State University 2071-9388 2542-1565 doi:10.24057/2071-9388-2015-8-1-4-15 https://doaj.org/article/b98cf9b177a24b2f961b6b50bd29b044 undefined Geography, Environment, Sustainability, Vol 8, Iss 1, Pp 4-15 (2015) evolution and dynamics of ice sheets analogies of the glaciological geological and atmospheric objects geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2015 fttriple https://doi.org/10.24057/2071-9388-2015-8-1-4-15 2023-01-22T19:27:17Z Complicated folded structures were recently recorded by radar survey in the lower portions of the Antarctic and Greenland ice sheets. From a geological point of view the Antarctic and Greenland ice sheets are considered as geological features, while the ice is classified as sedimentary or metamorphic rock. In this regard the genesis of the ice sheets is analyzed from the perspective of geodynamics and metamorphism, and complicated folded structures on radar profiles are interpreted as tectonic and metamorphic structures. This study considers the processes of three kinds of tectonic structures: glacial diapirs, glacial diapir folds and glacial intrusions. Radar profiles not only capture ice flow structure but can also detect the thermobaric field in ice sheet, and in this case the complicated folded structures are interpreted as representative of recorded metastable boundaries of ice recrystallization. Article in Journal/Newspaper Antarc* Antarctic Greenland Ice Sheet Unknown Antarctic Greenland The Antarctic GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY 8 1 4 15 |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
fttriple |
language |
English |
topic |
evolution and dynamics of ice sheets analogies of the glaciological geological and atmospheric objects geo envir |
spellingShingle |
evolution and dynamics of ice sheets analogies of the glaciological geological and atmospheric objects geo envir Alexey N. Markov Pavel G. Тalalay Dorthe Dahl-Jensen INTERPRETATIONS OF COMPLICATED FOLDED STRUCTURES AT THE LOWER PARTS OF ANTARCTIC AND GREENLAND ICE SHEETS |
topic_facet |
evolution and dynamics of ice sheets analogies of the glaciological geological and atmospheric objects geo envir |
description |
Complicated folded structures were recently recorded by radar survey in the lower portions of the Antarctic and Greenland ice sheets. From a geological point of view the Antarctic and Greenland ice sheets are considered as geological features, while the ice is classified as sedimentary or metamorphic rock. In this regard the genesis of the ice sheets is analyzed from the perspective of geodynamics and metamorphism, and complicated folded structures on radar profiles are interpreted as tectonic and metamorphic structures. This study considers the processes of three kinds of tectonic structures: glacial diapirs, glacial diapir folds and glacial intrusions. Radar profiles not only capture ice flow structure but can also detect the thermobaric field in ice sheet, and in this case the complicated folded structures are interpreted as representative of recorded metastable boundaries of ice recrystallization. |
format |
Article in Journal/Newspaper |
author |
Alexey N. Markov Pavel G. Тalalay Dorthe Dahl-Jensen |
author_facet |
Alexey N. Markov Pavel G. Тalalay Dorthe Dahl-Jensen |
author_sort |
Alexey N. Markov |
title |
INTERPRETATIONS OF COMPLICATED FOLDED STRUCTURES AT THE LOWER PARTS OF ANTARCTIC AND GREENLAND ICE SHEETS |
title_short |
INTERPRETATIONS OF COMPLICATED FOLDED STRUCTURES AT THE LOWER PARTS OF ANTARCTIC AND GREENLAND ICE SHEETS |
title_full |
INTERPRETATIONS OF COMPLICATED FOLDED STRUCTURES AT THE LOWER PARTS OF ANTARCTIC AND GREENLAND ICE SHEETS |
title_fullStr |
INTERPRETATIONS OF COMPLICATED FOLDED STRUCTURES AT THE LOWER PARTS OF ANTARCTIC AND GREENLAND ICE SHEETS |
title_full_unstemmed |
INTERPRETATIONS OF COMPLICATED FOLDED STRUCTURES AT THE LOWER PARTS OF ANTARCTIC AND GREENLAND ICE SHEETS |
title_sort |
interpretations of complicated folded structures at the lower parts of antarctic and greenland ice sheets |
publisher |
Lomonosov Moscow State University |
publishDate |
2015 |
url |
https://doi.org/10.24057/2071-9388-2015-8-1-4-15 https://doaj.org/article/b98cf9b177a24b2f961b6b50bd29b044 |
geographic |
Antarctic Greenland The Antarctic |
geographic_facet |
Antarctic Greenland The Antarctic |
genre |
Antarc* Antarctic Greenland Ice Sheet |
genre_facet |
Antarc* Antarctic Greenland Ice Sheet |
op_source |
Geography, Environment, Sustainability, Vol 8, Iss 1, Pp 4-15 (2015) |
op_relation |
2071-9388 2542-1565 doi:10.24057/2071-9388-2015-8-1-4-15 https://doaj.org/article/b98cf9b177a24b2f961b6b50bd29b044 |
op_rights |
undefined |
op_doi |
https://doi.org/10.24057/2071-9388-2015-8-1-4-15 |
container_title |
GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY |
container_volume |
8 |
container_issue |
1 |
container_start_page |
4 |
op_container_end_page |
15 |
_version_ |
1766268507547238400 |