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中国大陆东部强震区和火山区人工地震探测研究综述
引用本文:赖晓玲,孙译.中国大陆东部强震区和火山区人工地震探测研究综述[J].地球物理学进展,2006,21(3):722-729.
作者姓名:赖晓玲  孙译
作者单位:1.中国地震局地球物理勘探中心, 郑州 450002;2.华北水利水电学院,郑州 450008
基金项目:地震科学联合基金(104027,102025)资助,中国地震局地球物理勘探中心论著RCEG200507
摘    要:介绍了东北、华北、华东和华南的强震区和火山区的地震测深研究成果,揭示了强震区和火山区的地壳深部构造背景.分析表明,地壳深部断裂、中下地壳低速层、速度结构的差异、波速比异常、泊松比和岩性的不同、上地幔顶部隆起、莫霍界面较大的起伏、复杂的壳幔过渡带、滑脱构造、深部岩浆活动等构造特征与东部地区强震形成和发生有较为密切的关系.

关 键 词:中国东部  强震区  火山区  深地震测深  深部构造背景
文章编号:1004-2903(2006)03-0722-08
收稿时间:2005-10-10
修稿时间:2005-12-20

Review of deep seismic sounding in strong earthquake regions and volcanic regions of Eastern China
LAI Xiao-ling,SUN Yi.Review of deep seismic sounding in strong earthquake regions and volcanic regions of Eastern China[J].Progress in Geophysics,2006,21(3):722-729.
Authors:LAI Xiao-ling  SUN Yi
Institution:1. Geophysical Exploration Center , China Earthquake Administration, Zhengzhou 450002, China; 2. North China Institute of Water Conservancy and Hydroelectric Power, Zhengzhou 450008, China
Abstract:This paper briefly introduces deep seismic sounding results from strong earthquake regions and volcanic regions of Northeast China,North China,East China and South China.It reveals main crustal deep tectonic background in these regions.The analysis shows that several structural feature: deep fault in crust,the low velocity layer in the middle and lower crust,discrepancy of velocity structure,anomaly of velocity ratio,differ of Poisson ratio and lithology,top of upper mantle upheaval,larger fluctuation of Moho interface,complex crust-mantle transitional belt,detachment structure and deep magmation,are closely related with the formation and occurrence of strong earthquake in Eastern China.
Keywords:Eastern China  strong earthquake region  volcanic region  deep seismic sounding  deep tectonic background  
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