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青藏高原地球物理与大陆动力学研究的新进展

New research progress in geophysics and continental dynamics of the Tibetan Plateau

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【作者】 李秋生高原王绪本赵俊猛

【Author】 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;Institute of Earthquake Forecasting,China Earthquake Administration;Key Laboratory of Earth Exploration and Information Technique of Education Ministry(Chengdu University of Technology);Institute of Tibetan Plateau Research,Chinese Academy of Sciences;

【通讯作者】 高原;

【机构】 自然资源部深地动力学实验室(筹建),中国地质科学院地质研究所中国地震局地震预测研究所地球勘探与信息技术教育部重点实验室(成都理工大学)中国科学院青藏高原研究所

【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.

【Abstract】 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.

【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
  • 【文献出处】 地球物理学报 ,Chinese Journal of Geophysics , 编辑部邮箱 ,2020年03期
  • 【分类号】P31;P54
  • 【被引频次】17
  • 【下载频次】1048
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