Arid
DOI10.1016/j.quascirev.2019.04.019
The extent of permafrost during the Last Permafrost Maximum (LPM) on the Ordos Plateau, north China
Vandenberghe, Jef1; French, Hugh M.2,3,4; Jin, Huijun5,6; Wang, Xianyan7; Yi, Shuangwen7; He, Ruixia5
通讯作者Vandenberghe, Jef
来源期刊QUATERNARY SCIENCE REVIEWS
ISSN0277-3791
出版年2019
卷号214页码:87-97
英文摘要This paper presents new field observations that assist in further defining the extent of Last Permafrost Maximum (LPM) permafrost and frozen ground in north China. In that respect, this region is specific by its arid environment and continental position. Bedrock exposures and sand and gravel pits were examined along a south-north transect from southern Ordos as far as the vicinity of Dongsheng District, Ordos City on the Ordos Plateau (North China). Attention focussed upon the recognition of sand-wedge remains and possible cryoturbations. Two types of wedge structures were recognized: type A wedges extend to depths in excess of 3.0 m and are thought to have formed under conditions of continuous permafrost. Type B wedges are restricted to the upper 1.5 m and are thought to reflect discontinuous permafrost and/or deep seasonal frost. OSL dating of wedge infills indicates that type A wedges formed between 23-19 ka and younger type B wedges formed until the early Holocene. It is now possible to delineate a more exact position of the boundary between continuous permafrost and discontinuous permafrost and/or deep seasonal frost on the Ordos Plateau during the LPM. This boundaries occur between Dongsheng and Jinbian at 37 degrees-39 degrees N. (C) 2019 Elsevier Ltd. All rights reserved.
英文关键词Ordos China Dongsheng Permafrost Permafrost extent Sand wedge Sand-wedge cast Last permafrost maximum
类型Article
语种英语
国家Netherlands ; Canada ; Peoples R China
收录类别SCI-E
WOS记录号WOS:000471738800006
WOS关键词PLEISTOCENE PERMAFROST ; SINGLE-ALIQUOT ; INNER-MONGOLIA ; SAND WEDGES ; QUARTZ ; LUMINESCENCE ; RECORD ; TIME
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向Physical Geography ; Geology
来源机构中国科学院西北生态环境资源研究院 ; 南京大学
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/218273
作者单位1.Vrije Univ Amsterdam, Inst Earth Sci, Amsterdam, Netherlands;
2.Univ Ottawa, Dept Geog, Ottawa, ON, Canada;
3.Univ Ottawa, Dept Earth Sci, Ottawa, ON, Canada;
4.Univ Victoria, Dept Geog, Victoria, BC, Canada;
5.Chinese Acad Sci, Cold & Arid Reg Environm Engn Res Inst, State Key Lab Frozen Soils Engn, Lanzhou 730000, Gansu, Peoples R China;
6.Harbin Inst Technol, Sch Civil Engn, Harbin 150090, Heilongjiang, Peoples R China;
7.Nanjing Univ, Sch Geog & Ocean Sci, Nanjing 210023, Jiangsu, Peoples R China
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GB/T 7714
Vandenberghe, Jef,French, Hugh M.,Jin, Huijun,et al. The extent of permafrost during the Last Permafrost Maximum (LPM) on the Ordos Plateau, north China[J]. 中国科学院西北生态环境资源研究院, 南京大学,2019,214:87-97.
APA Vandenberghe, Jef,French, Hugh M.,Jin, Huijun,Wang, Xianyan,Yi, Shuangwen,&He, Ruixia.(2019).The extent of permafrost during the Last Permafrost Maximum (LPM) on the Ordos Plateau, north China.QUATERNARY SCIENCE REVIEWS,214,87-97.
MLA Vandenberghe, Jef,et al."The extent of permafrost during the Last Permafrost Maximum (LPM) on the Ordos Plateau, north China".QUATERNARY SCIENCE REVIEWS 214(2019):87-97.
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