共查询到20条相似文献,搜索用时 93 毫秒
1.
Surface deformation and gravity changes caused by dilatancy in a layered elastic-vis-coelastic half space 总被引:1,自引:0,他引:1
Surfacedeformationandgravitychangescausedbydilatancyinalayeredelastic┐vis┐coelastichalfspaceYONGWANG(王勇)HOUTSEHSU(许厚泽)Instit... 相似文献
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Fractal research of fault gouge 总被引:1,自引:0,他引:1
FractalresearchoffaultgougeSHUN-MEISHAO(邵顺妹)andJIN-CHANGZOU(邹瑾敞)EarthquakeResearchInstituteofLanzhou,StateSeismologicalBurea... 相似文献
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Seismicsourcerupturesofseveralstrongearthquakesof1989inSichuanregionofChinaYUANGAO1)(高原)ZHONG-LIANGWU2)(吴忠良)HUI-LANZHOU3)(周... 相似文献
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ThemechanismofregionalgravitychangesbeforeandaftertheTangshanearthquakeRUI-HAOLI(李瑞浩)JIAN-LIANGHUANG(黄建梁)HUILI(李辉)DONG-SHENG... 相似文献
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Effectsofmagnitudeaccuracyandcomplete┐nesdataonseismichazardparametersHUI-CHENGSHAO(邵辉成),JIA-SHUXIE(谢家树),PINGWANG(王平)andYA-X... 相似文献
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A preliminary research establishing the present-time intraplate blocks movement model on the Chinese
《地震学报(英文版)》1998,(4)
Apreliminaryresearchestablishingthepresent-timeintraplateblocksmovementmodelontheChinesemainlandbasedonGPSdataSHUO-YUZHOU1)(周... 相似文献
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LargescalecharacteristicdistancebetwenstrongearthquakeXIANFUDU(杜先富)SHAOXIEXU(许绍燮)InstituteofGeophysics,StateSeismologicalB... 相似文献
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AnalysisonrupturefeatureofagreatcomplicatedearthquakeinKamchatkaYUANGAO1)(高原)SIHUAZHENG1)(郑斯华)HUILANZHOU2)(周蕙兰)ZHENLIU2)(... 相似文献
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ResearchoncharacteristicsofmagnitudestructureofearthquakesequencesPEI-QINGSUN(孙佩卿)QIN-ZULI(李钦祖)YING-HUADAI(戴英华)JUNZHAO(赵军)Se... 相似文献
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UppermantleflowbeneaththeNorthwestofChinaanditslithosphericdynamicsJIAN-HUAHUANGI(黄建华);XIA-HUACHANGI(常筱华)andRONG-SHANFUI傅容珊)(... 相似文献
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Wang Ruobai 《中国地震研究》2005,19(3):327-337
INTRODUCTIONThe Zhangjiakou-Penglai fault zone has drawnextensive attentionfromseismologists and geologistssince it was determinedinthe1980’s(Zheng Binghua,et al.,1981).Ma Xingyuan,et al.(1989)consideredit asthe north boundaryof North China sub-block.Int… 相似文献
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ResearchofpatterndynamicsparametersofcrustaldeformationfieldinseismogenicprocessShuo-YuZHOU(周硕愚),YunWU(吴云),Ruo-BoWANG(王若柏)and... 相似文献
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Shi-Rong Mei 《地震学报(英文版)》1996,9(2):223-234
By studying the seismicity pattern before 37 earthquakes withM⩾6.0 in North China and the pattern of crustal deformation in the Capital Area from 1954 to 1992, some abnormal characteristics
of these patterns before strong earthquakes have been extracted. A comparison has been made between the anomalies of these
two kinds of patterns. From the results we can know the following. (1) Before a strong earthquake, the seismicity will strengthen
and the crustal deformation rate will increase. (2) Several years before a strong earthquake, there will be seismic gaps and
deformation gaps around the epicenter of the quake. (3) The dynamic parameters of patterns all show a decrease in information
dimension. This means that the crustal deformation has become more and more localized with time and it gives an important
indication showing that a strong earthquake is in preparation. At the end of the paper, the physical mechanisms of the abnormal
patterns of seismicity and crustal deformation have been explained in a unified way in terms of the earthquake-generating
model of a inhomogeneous strongbody in inhomogeneous media. 相似文献
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Shi-Rong Mei 《地震科学(英文版)》1996,9(2):223-234
By studying the seismicity pattern before 37 earthquakes withM?6.0 in North China and the pattern of crustal deformation in the Capital Area from 1954 to 1992, some abnormal characteristics of these patterns before strong earthquakes have been extracted. A comparison has been made between the anomalies of these two kinds of patterns. From the results we can know the following. (1) Before a strong earthquake, the seismicity will strengthen and the crustal deformation rate will increase. (2) Several years before a strong earthquake, there will be seismic gaps and deformation gaps around the epicenter of the quake. (3) The dynamic parameters of patterns all show a decrease in information dimension. This means that the crustal deformation has become more and more localized with time and it gives an important indication showing that a strong earthquake is in preparation. At the end of the paper, the physical mechanisms of the abnormal patterns of seismicity and crustal deformation have been explained in a unified way in terms of the earthquake-generating model of a inhomogeneous strongbody in inhomogeneous media. 相似文献
16.
Researchontemporalandspatialdistribu┐tion,evolutionarycharacterandmechanismofcrustaldeformationfieldbeforeandaftertheTangshan... 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
18.
华北北部地区的张家口-渤海断裂带是控制现代强震的一条地震构造带。新近纪以来,在区域NEE向主压应力的作用下,新发育了一系列的NE向构造活动带,与张家口-渤海断裂带组成1组共轭的剪切破裂系统,控制了近代强震的发生。文中主要探讨了这条断裂带的地壳形变特征。长趋势GPS地壳形变图像反映了这条活动断裂带相对完整的左旋走滑活动。分期的地壳形变图像揭示了在中强地震前,沿该断裂带出现一系列的NE向梯度异常带,分别指示了唐山-河间、三河-涞水以及延怀-山西地震构造活动带的活动,表明了沿张家口-渤海断裂带出现了中强地震的中期前兆。研究认为,强震前地壳形变揭示的是深部蕴震层的应变活动信息,而强震之后比较杂乱的图像特征体现了盖层的调整运动 相似文献
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地壳垂直形变速率梯度,断层形变速率变化与强震危险区研究 总被引:9,自引:2,他引:9
应用最新的全国垂直变形速率图和各地区不同年代的形变图。编绘相应的形变速率梯度图,计算了若干跨断层测量台、点资料的低通滤波残差及其一阶和二阶差分。结合在相应空间和时间域内所发 生的强震,讨论了地壳形变与强震的关系,得到了一些有意的结果。 相似文献