Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica
The typical glacial-marine sedimentation has been recorded from core NP93-2 in the Prydz Bay, Antarctica. The sedimentation processes, sedimentary environment and paleoclimate variations since 12937 a B.P. have been discussed, based on grain size, mineral composition and micropaleontological data, e...
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Polar Research Institute of China - PRIC
1996
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ftarcticportal:oai:generic.eprints.org:2119 2023-06-11T04:03:01+02:00 Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica Shiguo, Wu Youlang, Luo Youqiang, Wang Jun, Lu Fan, Zheng Shaoxian, Sun 1996-12 application/pdf http://library.arcticportal.org/2119/ http://library.arcticportal.org/2119/1/A602.007.pdf en eng Polar Research Institute of China - PRIC http://library.arcticportal.org/2119/1/A602.007.pdf Shiguo, Wu and Youlang, Luo and Youqiang, Wang and Jun, Lu and Fan, Zheng and Shaoxian, Sun (1996) Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica. Advances in Polar Science, 7 (2). pp. 164-172. Article PeerReviewed 1996 ftarcticportal 2023-04-19T22:52:31Z The typical glacial-marine sedimentation has been recorded from core NP93-2 in the Prydz Bay, Antarctica. The sedimentation processes, sedimentary environment and paleoclimate variations since 12937 a B.P. have been discussed, based on grain size, mineral composition and micropaleontological data, etc. The climate variation occurred at 10 ka, which expressed that there were increased inputs of terrigenous clastics. The climate change once again but temporarily took place at late Holocene. Article in Journal/Newspaper Advances in Polar Science Antarc* Antarctica Polar Science Polar Science Prydz Bay Arctic Portal Library Prydz Bay |
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Open Polar |
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Arctic Portal Library |
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ftarcticportal |
language |
English |
description |
The typical glacial-marine sedimentation has been recorded from core NP93-2 in the Prydz Bay, Antarctica. The sedimentation processes, sedimentary environment and paleoclimate variations since 12937 a B.P. have been discussed, based on grain size, mineral composition and micropaleontological data, etc. The climate variation occurred at 10 ka, which expressed that there were increased inputs of terrigenous clastics. The climate change once again but temporarily took place at late Holocene. |
format |
Article in Journal/Newspaper |
author |
Shiguo, Wu Youlang, Luo Youqiang, Wang Jun, Lu Fan, Zheng Shaoxian, Sun |
spellingShingle |
Shiguo, Wu Youlang, Luo Youqiang, Wang Jun, Lu Fan, Zheng Shaoxian, Sun Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica |
author_facet |
Shiguo, Wu Youlang, Luo Youqiang, Wang Jun, Lu Fan, Zheng Shaoxian, Sun |
author_sort |
Shiguo, Wu |
title |
Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica |
title_short |
Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica |
title_full |
Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica |
title_fullStr |
Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica |
title_full_unstemmed |
Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica |
title_sort |
holocene glacial-marine sedimentation in the prydz bay, antarctica |
publisher |
Polar Research Institute of China - PRIC |
publishDate |
1996 |
url |
http://library.arcticportal.org/2119/ http://library.arcticportal.org/2119/1/A602.007.pdf |
geographic |
Prydz Bay |
geographic_facet |
Prydz Bay |
genre |
Advances in Polar Science Antarc* Antarctica Polar Science Polar Science Prydz Bay |
genre_facet |
Advances in Polar Science Antarc* Antarctica Polar Science Polar Science Prydz Bay |
op_relation |
http://library.arcticportal.org/2119/1/A602.007.pdf Shiguo, Wu and Youlang, Luo and Youqiang, Wang and Jun, Lu and Fan, Zheng and Shaoxian, Sun (1996) Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica. Advances in Polar Science, 7 (2). pp. 164-172. |
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1768388695354769408 |