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Tracing Escaping Structure in the Northern Indo-China Peninsula by Openness and Remote Sensing

Tracing Escaping Structure in the Northern Indo-China Peninsula by Openness and Remote Sensing

作     者:Jie Zhang Qinglai Feng Zhi Zhang 

作者机构:State Key Laboratory of Geological Processes and Mineral ResourcesChina University of Geosciences Nanjing CenterChina Geological Survey School of Earth SciencesChina University of GeosciencesWuhan 

出 版 物:《Journal of Earth Science》 (地球科学学刊(英文版))

年 卷 期:2017年第28卷第1期

页      面:147-160页

核心收录:

学科分类:070904[理学-构造地质学] 0709[理学-地质学] 07[理学] 0708[理学-地球物理学] 0704[理学-天文学] 

基  金:supported by the National Natural Science Foundation of China (Nos.41172202,41190073,and 41402075) the China Geological Survey (No.1212011121256) the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan (No.MSFGPMR201502) 

主  题:Openness Indo-China Peninsula escaping structure remote sensing. 

摘      要:The Openness based on DEM emphasizes the terrain convexity and concavity. It facilitates the interpretation of detailed landforms on the Earth's surface. Compared with the layer stacking of ETM+ with less three-dimensionality and visualizability and with indefinite details of linear images in the deep cutting or deep covered region, the Openness is used for accurate interpretation of tectonic geomorphic units and linear structures. In this paper, the ETM+ images(741 RGB) and RRIM based on Openness combined with the field geological investigation are used to trace the escaping structure in SE Asia. The east boundary is Ailaoshan shear zone and the west boundary is Uttaradit-Dien Bien Phu fault, which together form the southwards extruding wedge block. The arc boundary surface of the southern Khorat Plateau is jutted to the north. The NW and NE sides of Khorat Plateau are traversed by Uttaradit-Dien Bien Phu fault and Thakhek-Da Nang fault, respectively, resulting in a blocked escaping structure. The SE margins of Truong Son structure belt and Song Ma structure belt are both arcs jutting to SE. These arc structures clamped by faults or related to the fault on one side indicating the material flow direction obviously, are the most specific manifestation of escaping structures. Moreover, these push units are extruded from south to north successively.

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