阿尔金断裂中段15Ma左右的应变集中:来自高精度地震反射的证据
The Altyn Tagh system is commonly thought to initiate in the early Cenozoic;however,when purestrike-slip motion occurred on its main trace,the Altyn Tagh Fault (ATF),remains an unsolved question.Tosolve this problem,we studied the integrated deformation history in the northwestern margin of the QaidamBasin next to the ATF based on newly-obtained high-resolution seismic reflection data.The result reveals aseries of basement-involved reverse faults merging the ATF at depth and constituting a 20 – 50 km fault zonesub-parallel to the ATF.
阿尔金断裂 变形特征 地震反射数据
吴磊 赵海锋 肖安成 沈亚
浙江大学地球科学学院 杭州 310027 中石油东方地球物理公司 涿州 072750
国内会议
北京
中文
953-953
2015-10-11（万方平台首次上网日期，不代表论文的发表时间）