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中国大陆邻区的地震活动和中国大陆地震的关系 总被引:1,自引:0,他引:1
研究了3个方面的问题,一是中国大陆周边4个地震带地震活跃期与中国大陆地震活跃期的准同步性和它们目前的活动水平;二是欧亚地震带西部与中国大陆的地震活动呈出现明显的超前或滞后性;三是中国大陆邻区6个地震区的强震与中国大陆活跃期的开始或与中国大陆强震的对应关系。 相似文献
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自1988年11月唐古拉山7级地震及澜沧-耿马7.6与7.2级地震以后,1990年4月26日青海共和发生了7级地震,至今中国大陆已有两年半的时间未发生7级地震了。而同一时期,中国西部周缘地区7级强震却很活跃。 相似文献
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冀鲁豫交界区地震活动与区域构造运动的关系 总被引:1,自引:0,他引:1
根据冀鲁豫交界区(35.0°-36.5°N,113.5°-116.0°E)的地震构造格架与地震活动分布,分析研究了本区的地震活动性,得出了本区地震活动与区域构造运动的牵动作用,并探讨了本区的地震危险性。 相似文献
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1.1989年地震活动概况 今年我国大陆至今未发生7级以上地震,但发生7次6级以上地震,其中6次在西南地区,表明大陆地震活动仍处在起伏活跃中,西部乃是主体活动地区。 1989年1—10月,新疆境内发生的地震3.0—3.9级(M_S下同)138次,4.0—4.9级26次,5.0—5.1级3次。地震活动明显低于平均水平。地震活动主要集中于西昆仑地震带、乌恰地区和南天山地震带。北天山地震带继续相对平静。 相似文献
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Establishment of the GPS Monitoring Network in North China, the Relation of Horizontal Crustal Movement to Stress Field and Seismicity 总被引:1,自引:0,他引:1
Li Yanxing Hu Xinkang Zhao Chengkun Wang Min Guo Liangqian and Xu JushengFirst Crustal Deformation Monitoring Center China Seismological Bureau Tianjin China Institute of Seismology China Seismological Bureau Wuhan China 《中国地震研究》1998,(4)
In the paper, the establishment, measurement, data-processing program and monitoring accuracy of the GPS seismic monitoring network in North China, especially in the Capital-Circle area, have been presented briefly. The relation of horizontal crustal deformation to tectonic movement, stress-field variation and seismicity has been analyzed in detail. The results indicate that the accuracy of GPS measurement has reached the order of 10-9 and the annual rate of horizontal crustal deformation in North China is about 4 ~5 mm. Horizontal crustal movement is a direct indication of the regional stress field. Therefore, by monitoring the time-sequence variation of horizontal crustal motion, it would be possible to investigate the change in the stress field, to analyze the tendency of seismicity and to determine the seismogenic zones. 相似文献
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In order to study the present crustal movement and geodynamics in China‘s continent, a countrywide GPS monitoring network consisting of 22 stations was set up evenly on major tectonic blocks in China‘s continent in the early 1990s. Three-phase observations using the network were carried out in 1992, 1994, and 1996, respectively. In this paper, the data processing and accuracy of the three-phase observations are examined and the basic characteristics of present block movement in China‘s continent are analyzed based on the data of three-phase repeated observations. The study result indicates that the accuracy of data obtained in three-phase observations on the GPS network reaches 10-8 ~ 10-9, which is adequate to the need of monitoring of crustal movement. A model for block movement in China‘s continent constructed based on the result of the three-phase observations has effectively tested the results of geological and geophysical studies. In global framework, China‘s continent as a whole shows its clear eastward motion and its regional movement relative to Siberian block is characterized by that the western China is mainly affected by northward subduction and pushing of Indian Plate. Qinghai-Xizang Plateau shows clear eastward lateral slip simultaneously with longitudinal compression. It is more favorable to the escape model for the continent. Block movement of eastern China is under the combined effect of Indian, Pacific,and Philippine plates, resulting in northeastern and eastern motions of eastern China up to southeastern coastal region where the effect of Philippine Plate strengthens. 相似文献
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岛弧构造的垂直形变场与水平位移场及其构造运动和地震活动特征 总被引:1,自引:0,他引:1
本文根据水平构造应力作用,推导了弧形构造的理论垂直形变场、水平位移场和应力场,进而对全球性的岛弧构造带在构造运动、地震活动和震源机制等方面的特征给出了新的解释;提出岛弧等弧形构造主要是在弧形构造位移场、应力场作用下逐渐形成的,而大洋板块的俯冲作用是次要的。 相似文献
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INTRODUCTIONThe 3Ichuan-Yunnan region Is located at the southeastern edg6d Qinghal-Xlzang plate。 Theco-function between east-towhwhs。yementdthe cmstal substances In Qinghal-Xlzang and wedging ofAssmann acme has m扣e the re9onal tectonic activity very co呷floated since Cenozolc.TheNeotectonlc deformation and earthquake activity re verystrong In the place where Is the most activeegion of strong ea耐hqUqU拙es In China s Continent.Thestudy of neotectonlc movement,selsmogeol… 相似文献
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地电阻率1年尺度异常时空丛集现象与地震活动性 总被引:7,自引:0,他引:7
研究了我国23°~47°N、86°~127°E范围内92个地电台、207个测道自建台至1997年的地电阻率变化,得到以下认识(1)1976、1980~1981、1985~1986、1988、1991、1994年和1997年全国范围45.0%~58.0%的地电台显示1年尺度地电阻率异常(以下简称"异常高潮期").异常高潮期与大陆及周边Ms≥7.1强震活动,Ms≥5.0地震丛集活动、地球自转加速年份和减速过程中明显趋于加速的年份相对应;西北、西南和华北-东北各区异常高潮期主要集中在上述年份,与各区内Ms≥5.0地震丛集活动的年份明显对应.这表明地电阻率异常确实反应了地壳力学状态变化,地电阻率观测在地震预报中有实际意义.(2)1974~1997年的24年中,映震异常占异常总数的38.27%,无震异常占61.73%,表明地电阻率观测场兆相当丰富.(3)地球自转加速年份和减速过程中明显趋于加速年份中大陆边界动力加强,促成了地电阻率异常高潮期、Ms≥7.1强震活动、Ms≥5.0地震丛集活动年份之间的对应关系;中国大陆及区域性应力、构造、介质等条件对显示异常、强震活动、Ms≥5.0地震丛集活动起了积极作用.(4)地电阻率异常高潮期与地震活动性、地球自转速度变化明显对应;强震周围异常"时空强"演化与活动构造和发震机制有一定关系.这两方面结果有助于认识异常时空强演化的复杂性.(5)全国范围地电阻率异常高潮年份中,我国大陆西部地震活动水平明显高于东部. 相似文献
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川滇地区强地震活动与区域新构造运动的关系 总被引:33,自引:0,他引:33
在分析了川滇地区强震活动空间分布的非均匀性图象、震源破裂图象及震源断层力学性质等资料的基础上,讨论了该地区强震活动与区域活动断裂、活动地块现今运动状态、深部介质构造环境等的关系,对该区强震活动特征及其可能的力学机制进行了讨论. 相似文献
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Xu Wenjun Zhao Weiming Chai Chizhang Jin Yanlong Sun Lixin Zheng Sihu Satoshi Miura 《中国地震研究》2001,15(3):252-265
INT正ODU**!0厂Nln以la Is located In the nol’th segmentdthe North-southselsnuc Belt,Whlchls thejuncturedthe Qinghai-Xizang(Dbet)block,Alxa block and Odos block.In that region,the tectonic activity。svery strong;。y strong earthquakes occu。d In history,such as the 1739 ingluo M。8.0 earthqu拙eandl920 Halyuan M。8.5 eafthquake,etc.; Merately strongeaFthquakes are still veryactlve atpresent,onlyln the Wuzhong-un斟m area,there have been7 e血hquakes tvlth M。>5.0 to occ… 相似文献