Geology of Fildes Peninsula, King George Island
On the basis of the geological mapping, isotopic choronoogcal and petrological evidences, the authors suggested that the early Tertiary volcanic strata in the Fildes Peninsula could be divided into two formations and four members. The erupted centers in the peninsula were gradually migrating from th...
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Polar Research Institute of China - PRIC
1990
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Online Access: | http://library.arcticportal.org/2017/ http://library.arcticportal.org/2017/1/A19900102.pdf |
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ftarcticportal:oai:generic.eprints.org:2017 2023-05-15T17:03:46+02:00 Geology of Fildes Peninsula, King George Island Xiangshen, Zheng Xiaohan, Liu 1990-12 application/pdf http://library.arcticportal.org/2017/ http://library.arcticportal.org/2017/1/A19900102.pdf en eng Polar Research Institute of China - PRIC http://library.arcticportal.org/2017/1/A19900102.pdf Xiangshen, Zheng and Xiaohan, Liu (1990) Geology of Fildes Peninsula, King George Island. Advances in Polar Sciences, 1 (1). pp. 8-19. Article PeerReviewed 1990 ftarcticportal 2023-04-05T22:52:04Z On the basis of the geological mapping, isotopic choronoogcal and petrological evidences, the authors suggested that the early Tertiary volcanic strata in the Fildes Peninsula could be divided into two formations and four members. The erupted centers in the peninsula were gradually migrating from the western coast to the eastern and the subvolcanic intrusives were regularly distributed along a series of NWW-SEE trending faults. All of these were basically formed in two stages of volcanic activities from Paleocene to Eocene. Article in Journal/Newspaper King George Island Arctic Portal Library Fildes ENVELOPE(-58.817,-58.817,-62.217,-62.217) Fildes peninsula ENVELOPE(-58.948,-58.948,-62.182,-62.182) King George Island |
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Open Polar |
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Arctic Portal Library |
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ftarcticportal |
language |
English |
description |
On the basis of the geological mapping, isotopic choronoogcal and petrological evidences, the authors suggested that the early Tertiary volcanic strata in the Fildes Peninsula could be divided into two formations and four members. The erupted centers in the peninsula were gradually migrating from the western coast to the eastern and the subvolcanic intrusives were regularly distributed along a series of NWW-SEE trending faults. All of these were basically formed in two stages of volcanic activities from Paleocene to Eocene. |
format |
Article in Journal/Newspaper |
author |
Xiangshen, Zheng Xiaohan, Liu |
spellingShingle |
Xiangshen, Zheng Xiaohan, Liu Geology of Fildes Peninsula, King George Island |
author_facet |
Xiangshen, Zheng Xiaohan, Liu |
author_sort |
Xiangshen, Zheng |
title |
Geology of Fildes Peninsula, King George Island |
title_short |
Geology of Fildes Peninsula, King George Island |
title_full |
Geology of Fildes Peninsula, King George Island |
title_fullStr |
Geology of Fildes Peninsula, King George Island |
title_full_unstemmed |
Geology of Fildes Peninsula, King George Island |
title_sort |
geology of fildes peninsula, king george island |
publisher |
Polar Research Institute of China - PRIC |
publishDate |
1990 |
url |
http://library.arcticportal.org/2017/ http://library.arcticportal.org/2017/1/A19900102.pdf |
long_lat |
ENVELOPE(-58.817,-58.817,-62.217,-62.217) ENVELOPE(-58.948,-58.948,-62.182,-62.182) |
geographic |
Fildes Fildes peninsula King George Island |
geographic_facet |
Fildes Fildes peninsula King George Island |
genre |
King George Island |
genre_facet |
King George Island |
op_relation |
http://library.arcticportal.org/2017/1/A19900102.pdf Xiangshen, Zheng and Xiaohan, Liu (1990) Geology of Fildes Peninsula, King George Island. Advances in Polar Sciences, 1 (1). pp. 8-19. |
_version_ |
1766057710671888384 |