The Geomorphologic Process of the Diamicton in Jinpingzi in the Valley of Jinsha River,China
The Geomorphologic Process of the Diamicton in Jinpingzi in the Valley of Jinsha River,China
摘要
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
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
出处
《地学前缘》
EI
CAS
CSCD
北大核心
2009年第S1期45-45,共1页
Earth Science Frontiers
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