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青藏高原地球物理与大陆动力学研究的新进展 被引量:17

New research progress in geophysics and continental dynamics of the Tibetan Plateau
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摘要 岩石圈地球物理探测、深部结构成像与各向异性等研究是青藏高原大陆动力学研究的基础.近年来,随着深部地球物理探测技术和反演成像技术的进步,信息提取与细节分辨能力不断提升,青藏高原壳幔结构、碰撞和隆升动力学、资源与地质灾害的深部机制等研究进展显著.本专辑收录33篇论文,主要分布在深部结构与地球物理探测、地震各向异性与变形、断裂性质与地震活动等三个主要研究领域.本文重点围绕这些论文,对近年来青藏高原地球物理研究进展进行综述. Lithospheric geophysical exploration,structural imaging and anisotropy are the basis for the study of continental dynamics of the Tibetan Plateau.In recent years,with the advancement of deep geophysical exploration technology and inversion imaging technology,and the continuous improvement of information recognition and resolution,researches on crust-mantle structure,dynamics of collision and uplift,and deep mechanics of resource and geological hazards in the Tibetan Plateau have made remarkable progress.The 33 papers in this special issue are mainly distributed in three major research fields,i.e.the deep structure and geophysical exploration,the seismic anisotropy and deformation,the fault and seismicity.Based on the papers in this special issue,this review makes comments on research progress of geophysics of the Tibetan Plateau.
作者 李秋生 高原 王绪本 赵俊猛 LI QiuSheng;GAO Yuan;WANG XuBen;ZHAO JunMeng(Institute of Geology,Chinese Academy of Geological Sciences,Key Laboratory of Deep-Earth Dynamics(in building),Ministry of Nature Resources,Beijing 100037,China;Institute of Earthquake Forecasting,China Earthquake Administration,Beijing 100036,China;Key Laboratory of Earth Exploration and Information Technique of Education Ministry(Chengdu University of Technology),Chengdu 610059,China;Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China)
出处 《地球物理学报》 SCIE EI CAS CSCD 北大核心 2020年第3期789-801,共13页 Chinese Journal of Geophysics
基金 国家重点研发计划(2016YFC0600302,2017YFC1500304) 国家自然科学基金项目(41574092,41730212)共同资助
关键词 青藏高原 地球物理探测 地壳-上地幔结构 深部构造 变形 断裂 地震 Tibetan Plateau Geophysical exploration Crust-upper mantle structure Deep tectonics Deformation Fault Earthquake
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