Relationship between the distribution of periglacial landforms and glaciation history, Fildes Peninsula, King George Island, Antarctica
Three kinds of profile assemblage features show that periglacial landforms have an internal relationship in genesis. For example, where there is a rich weathering debris, the dominant landforms are talus, black slopes, mass movement features, and mega-grained sorted forms. Where the debris material...
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permafrost and periglacial processes
1996
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ftpekinguniv:oai:localhost:20.500.11897/402835 2023-05-15T13:53:16+02:00 Relationship between the distribution of periglacial landforms and glaciation history, Fildes Peninsula, King George Island, Antarctica Zhu, C Cui, ZJ Zhang, JX Zhu, C (reprint author), NANJING UNIV,DEPT EARTH & OCEAN SCI,NANJING 210093,PEOPLES R CHINA. BEIJING UNIV,DEPT GEOG,BEIJING 100871,PEOPLES R CHINA. NANJING UNIV,DEPT EARTH & OCEAN SCI,NANJING 210093,PEOPLES R CHINA. 1996 https://hdl.handle.net/20.500.11897/402835 https://doi.org/10.1002/(SICI)1099-1530(199601)7:1<95::AID-PPP206>3.3.CO;2-V en eng permafrost and periglacial processes PERMAFROST AND PERIGLACIAL PROCESSES.1996,7,(1),95-100. 1025991 1045-6740 http://hdl.handle.net/20.500.11897/402835 doi:10.1002/(SICI)1099-1530(199601)7:1<95::AID-PPP206>3.3.CO;2-V WOS:A1996UQ30500007 SCI periglacial landforms Antarctica glaciation Journal 1996 ftpekinguniv https://doi.org/20.500.11897/402835 https://doi.org/10.1002/(SICI)1099-1530(199601)7:1<95::AID-PPP206>3.3.CO;2-V 2021-08-01T10:27:00Z Three kinds of profile assemblage features show that periglacial landforms have an internal relationship in genesis. For example, where there is a rich weathering debris, the dominant landforms are talus, black slopes, mass movement features, and mega-grained sorted forms. Where the debris material is silty, fine-grained periglacial forms (for example, gelifluction steps and striated soils) dominate. Where the debris source is limited, talus only appears at the south-east side of periglacial tors and hilltops; the major periglacial forms are striated soils and muddy sorted circles. In general, periglacial landforms show a difference between stoss and leeward slopes. Geography, Physical Geology SCI(E) 2 ARTICLE 1 95-100 7 Journal/Newspaper Antarc* Antarctica King George Island Permafrost and Periglacial Processes Peking University Institutional Repository (PKU IR) Fildes ENVELOPE(-58.817,-58.817,-62.217,-62.217) Fildes peninsula ENVELOPE(-58.948,-58.948,-62.182,-62.182) King George Island |
institution |
Open Polar |
collection |
Peking University Institutional Repository (PKU IR) |
op_collection_id |
ftpekinguniv |
language |
English |
topic |
periglacial landforms Antarctica glaciation |
spellingShingle |
periglacial landforms Antarctica glaciation Zhu, C Cui, ZJ Zhang, JX Relationship between the distribution of periglacial landforms and glaciation history, Fildes Peninsula, King George Island, Antarctica |
topic_facet |
periglacial landforms Antarctica glaciation |
description |
Three kinds of profile assemblage features show that periglacial landforms have an internal relationship in genesis. For example, where there is a rich weathering debris, the dominant landforms are talus, black slopes, mass movement features, and mega-grained sorted forms. Where the debris material is silty, fine-grained periglacial forms (for example, gelifluction steps and striated soils) dominate. Where the debris source is limited, talus only appears at the south-east side of periglacial tors and hilltops; the major periglacial forms are striated soils and muddy sorted circles. In general, periglacial landforms show a difference between stoss and leeward slopes. Geography, Physical Geology SCI(E) 2 ARTICLE 1 95-100 7 |
author2 |
Zhu, C (reprint author), NANJING UNIV,DEPT EARTH & OCEAN SCI,NANJING 210093,PEOPLES R CHINA. BEIJING UNIV,DEPT GEOG,BEIJING 100871,PEOPLES R CHINA. NANJING UNIV,DEPT EARTH & OCEAN SCI,NANJING 210093,PEOPLES R CHINA. |
format |
Journal/Newspaper |
author |
Zhu, C Cui, ZJ Zhang, JX |
author_facet |
Zhu, C Cui, ZJ Zhang, JX |
author_sort |
Zhu, C |
title |
Relationship between the distribution of periglacial landforms and glaciation history, Fildes Peninsula, King George Island, Antarctica |
title_short |
Relationship between the distribution of periglacial landforms and glaciation history, Fildes Peninsula, King George Island, Antarctica |
title_full |
Relationship between the distribution of periglacial landforms and glaciation history, Fildes Peninsula, King George Island, Antarctica |
title_fullStr |
Relationship between the distribution of periglacial landforms and glaciation history, Fildes Peninsula, King George Island, Antarctica |
title_full_unstemmed |
Relationship between the distribution of periglacial landforms and glaciation history, Fildes Peninsula, King George Island, Antarctica |
title_sort |
relationship between the distribution of periglacial landforms and glaciation history, fildes peninsula, king george island, antarctica |
publisher |
permafrost and periglacial processes |
publishDate |
1996 |
url |
https://hdl.handle.net/20.500.11897/402835 https://doi.org/10.1002/(SICI)1099-1530(199601)7:1<95::AID-PPP206>3.3.CO;2-V |
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 |
Antarc* Antarctica King George Island Permafrost and Periglacial Processes |
genre_facet |
Antarc* Antarctica King George Island Permafrost and Periglacial Processes |
op_source |
SCI |
op_relation |
PERMAFROST AND PERIGLACIAL PROCESSES.1996,7,(1),95-100. 1025991 1045-6740 http://hdl.handle.net/20.500.11897/402835 doi:10.1002/(SICI)1099-1530(199601)7:1<95::AID-PPP206>3.3.CO;2-V WOS:A1996UQ30500007 |
op_doi |
https://doi.org/20.500.11897/402835 https://doi.org/10.1002/(SICI)1099-1530(199601)7:1<95::AID-PPP206>3.3.CO;2-V |
_version_ |
1766258296946163712 |