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DOI10.1016/j.geomorph.2019.05.013
Alluvial plains formation in response to 100-ka glacial-interglacial cycles since the Middle Pleistocene in the southern Tian Shan, NW China
Huang, Weiliang; Yang, Xiaoping; Jobe, Jessica A. Thompson; Li, Shengqiang; Yang, Haibo; Zhang, Lin
发表日期2019-09-15
ISSN0169-555X
EISSN1872-695X
卷号341页码:86-101
英文摘要The tenet of the Milankovitch theory is that Northern Hemisphere solar insolation, controlled by Earth's orbital is responsible for cyclic climate variations. Eccentricity in this context is responsible for cyclic variability of 100 ka and may drive p
关键词Be-10 depth-profilesGlacial-interglacial cyclesTian Shan100 ka-eccentricity Milankovitch cycle
学科领域Geography, Physical;Geosciences, Multidisciplinary
语种英语
WOS记录号WOS:000476965100007
来源期刊GEOMORPHOLOGY
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/79998
作者单位Changan Univ, Coll Geol Engn & Surveying, Xian 710054, Shaanxi, Peoples R China
推荐引用方式
GB/T 7714
Huang, Weiliang,Yang, Xiaoping,Jobe, Jessica A. Thompson,et al. Alluvial plains formation in response to 100-ka glacial-interglacial cycles since the Middle Pleistocene in the southern Tian Shan, NW China[J],2019,341:86-101.
APA Huang, Weiliang,Yang, Xiaoping,Jobe, Jessica A. Thompson,Li, Shengqiang,Yang, Haibo,&Zhang, Lin.(2019).Alluvial plains formation in response to 100-ka glacial-interglacial cycles since the Middle Pleistocene in the southern Tian Shan, NW China.GEOMORPHOLOGY,341,86-101.
MLA Huang, Weiliang,et al."Alluvial plains formation in response to 100-ka glacial-interglacial cycles since the Middle Pleistocene in the southern Tian Shan, NW China".GEOMORPHOLOGY 341(2019):86-101.
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