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雅鲁藏布江下游阶地特征及其工程意义
引用本文:扶敏,詹涛,谢超. 雅鲁藏布江下游阶地特征及其工程意义[J]. 四川建材, 2019, 0(5): 74-75
作者姓名:扶敏  詹涛  谢超
作者单位:重庆市地质矿产勘查开发局107地质队;重庆江北地质工程勘察院;中国地震局第二监测中心
摘    要:雅鲁藏布江下游出露有T1和T2阶地剖面,均为基座阶地。简要介绍了出露阶地的组分及沉积特征,并根据墨脱县境内阶地的时代获得了雅鲁藏布江下游区域的下切速率,结合区域所受气候及地貌形态,评价了区域地壳稳定性,并对场地的建设适宜性进行了分析。

关 键 词:雅鲁藏布江下游  阶地  构造隆升  稳定性评价

Terracefeature of the downstream region of YarluZangbu river and its engineering signicance
Affiliation:(107 Geological Team,Chongqing Bureau of Geology and Minerals Exploration,Chongqing 401120,China;Chongqingjiangbei Institute of Geo - Engineering Investigation,Chongqing 401120,China;The Second Monitoring and Application Center,China Earthquake Administration,Xi?an 710054,China)
Abstract:FU Min;ZHAN Tao(107 Geological Team,Chongqing Bureau of Geology and Minerals Exploration,Chongqing 401120,China;Chongqingjiangbei Institute of Geo - Engineering Investigation,Chongqing 401120,China;The Second Monitoring and Application Center,China Earthquake Administration,Xi?an 710054,China)
Keywords:downstream of the Yarlu Zangbu River  terrace  tectonic uplift  estimation of stability
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