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榆木山北缘断裂现今构造活动特征及其对青藏高原北东扩展的构造地貌响应
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陈干1, 郑文俊2,*, 王旭龙3, 张培震1,2, 熊建国2, 俞晶星1,4, 刘兴旺5, 毕海芸1, 刘金瑞1, 艾明1 |
PRESENT KINEMATICS CHARACTERISTICS OF THE NORTHERN YUMUSHAN ACTIVE FAULT AND ITS RESPONSE TO THE NORTHEASTWARD GROWTH OF THE TIBETAN PLATEAU
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CHEN Gan 1, ZHENG Wen-jun 2, WANG Xu-long 3, ZHANG Pei-zhen 1,2, XIONG Jian-guo 2, YU Jin-xing 1,4, LIU Xing-wang 5, BI Hai-yun 1, LIU Jin-rui 1, AI Ming 1
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骆驼城陡坎不是断层陡坎的证据 a1 “断层面”两侧地层采集光释光样品, a2 剖面地层单元示意图; b1 古代防洪堤岸加高的证据(至少3次),下部层位连续, b2 剖面地层单元示意图; c 上部表现断层面形态,下部层位无错动; d 古代水渠的完整形态 |
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