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Permeability and Sedimentation Characteristics of Pleistocene Fluvio-glacial Deposits in the Dadu River Valley, Southwest China
TU Guo-xiang; HUANG Run-qiu; DENG Hui; LI Yan-rong
2013
页码482-493
关键词冰川沉积物 中国西南地区 大渡河流域 沉积特征 渗透性 更新世 河湖 晶粒尺寸分布
URL标识查看原文
内容类型期刊论文
URI标识http://www.corc.org.cn/handle/1471x/3729858
专题成都理工大学
作者单位1.[1]State Key Laboratory of Geo-hazard Prevention and Geo-environment Protection, Chengdu University of Technology,Chengdu 61oo59, China
2.[2]Department of Earth Sciences, The University of Hong Kong, Hong Kong, China
推荐引用方式
GB/T 7714
TU Guo-xiang,HUANG Run-qiu,DENG Hui,et al. Permeability and Sedimentation Characteristics of Pleistocene Fluvio-glacial Deposits in the Dadu River Valley, Southwest China[J],2013:482-493.
APA TU Guo-xiang,HUANG Run-qiu,DENG Hui,&LI Yan-rong.(2013).Permeability and Sedimentation Characteristics of Pleistocene Fluvio-glacial Deposits in the Dadu River Valley, Southwest China.,482-493.
MLA TU Guo-xiang,et al."Permeability and Sedimentation Characteristics of Pleistocene Fluvio-glacial Deposits in the Dadu River Valley, Southwest China".(2013):482-493.
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