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The Geomorphologic Process of the Diamicton in Jinpingzi in the Valley of Jinsha River,China
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作者 Qinmian Xu~1,Dayuan Yang~2,Zhaoshuai Ge~3 1.Tianjin Institute of Geology and Mineral Resources,Tianjin 300170,China. 2.School of Geographic and Oceanographic Sciences,Nanjing University,Nanjing 210093,China 3.School of Urban and Environmental Sciences,Xuzhou Normal University,Xuzhou 221116,China 《地学前缘》 EI CAS CSCD 北大核心 2009年第S1期45-45,共1页
The diamicton of Jinpingzi,which looks like a slide according to morphological character,lies on the Kangdian tectonic zone.According as geomorphologic, sedimentary characteristics and stratigraphy of the diamicton of... The diamicton of Jinpingzi,which looks like a slide according to morphological character,lies on the Kangdian tectonic zone.According as geomorphologic, sedimentary characteristics and stratigraphy of the diamicton of Jinpingzi,there are three geomorphologic processes,which are accumulation and sidesway(197-137 ka B.P.),divagation and incision(137-41ka B.P.) and intensity 展开更多
关键词 the Jinsha River:diamicton LATE medio-pleistocene geomorphic PROCESS
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