共查询到19条相似文献,搜索用时 187 毫秒
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本文依据深部地球物理场、区域大地构造、地表活动断裂、地震活动等,划分了中国大陆的地震构造带,同时分析了地震构造带的活动特征和孕震构造条件,在此基础上,具体地把地震构造带的概念应用于地震危险区分析之中,探讨了地震危险区及地震前兆异常与地震构造带的关系,本文提出以地震构造带研究作为地震监测和预报工作的基础,将地震构造带作为系统性的活动构造条件应用于地震危险区划分之中。 相似文献
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哈萨克斯坦地震活动造山带由从南东环绕年轻板块─—图兰板块和哈萨克地质构造的山体构成。仅在最近的107年这里发生了10余次强烈的破坏性的M≥6.5级的地震。因此,最近20年进行的地震研究的方向是查明地震活动与地壳构造系统和构造过程的关系。一般情况下最重要的地震构造问题是确定强烈地震的地点,同时确定在“地点”下面的无论是区域的还是局部的震源分布。地震的构造研究还包括一系列问题:区域地震活动性、加固地基、新构造运动、最新构运、古地震断层、查明估计地壳地震势能的定量标准等等。本文主要研究了区域地震活动性与地震构造基础的可比性和造山带的地震断层,根据地质条件估计了地壳的地震势能;认为,地震构造图可以作为估计地震危险的基础。 相似文献
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淮河流域中强震活动区的地震构造背景 总被引:1,自引:0,他引:1
介绍了沿淮河干流展布的淮河构造变形带的断裂构造特征,分析了该构造变形带内中强地震与断层构造的关系,并结合淮河流域地球物理场资料的分析,提出了中强地震发生的地震地质标志。 相似文献
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成都平原最大可能地震能力估计 总被引:4,自引:1,他引:4
成都平原位于青藏高原的东南缘,紧靠龙门山推覆构造带。近代地壳运动,断裂活动和地震活动水平应介于青藏高原活动构造区和四川盆地弱活动构造区的过渡地带。本文从构造类比角度对成都平原的最大可能地震能力进行了评估;结果表明其最大可能地震能力高于该区的地震史载水平。其中,蒲江-新津-成都德阳断裂可达6±0.5级,大邑-彭县-绵竹隐伏断裂可达5.6级左右。 相似文献
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前兆异常动态扫描与区域构造活动背景结合的研究--试建立华北地区构造活动性与地震危险性综合评估数字化图 总被引:2,自引:0,他引:2
为实现前兆异常空间扫描与构造活动背景的有机结合,本文提出:以近效十年2级以上地震的累计频次分布为依据,量化评估华北各构造区现今活动状态与基本活动水平,以近千年来的5级以上地震的年均发生率分布为依据量化评估断裂构造(带、段)的地震活动危险性,并将上述两项量化评估的数值分布图进行叠加,建立起标示华北地区现今构造活动与地震危险性的数字化图,以此作为前兆异常空间扫描的输入,从而增强前兆空间扫描图像中的构造活动信息及其异常演化特征,提高强震危险预测的能力。 相似文献
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华北地区的共轭地震构造带 总被引:10,自引:3,他引:10
本文采用小地震活动图象和4.0级(Ms)以上地震震源机制资料的构造分析方法,得到一幅华北地区震源构造在地面的投影分布图,它显示4条NNE-NE向和1条NWW-NW向地震构造带交切成的共轭剪切构造格架。每条地震构造带又由一系列共轭剪切构造组成。由发生在带内的5个大震序列共轭破裂特征发现,共轭地震构造的孕震与控震作用是地震构造带形成的机制。 相似文献
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Li Yingzhen 《中国地震研究》2006,20(2):174-189
INTRODUCTIONStudy on active tectonics shows that large earthquake in seismogenic tectonics will recur in situperiodically.These large earthquakes that recur periodically are called“characteristic earthquakes”.( Wallace , et al ., 1984 ; Nishenko, 1987) . However , several sub-strong earthquakes and manymoderate-small earthquakes will occur in the interval between two temporally adjacent characteristicearthquakes,i .e .in a complete recurrence cycle (Shen Jun,et al .,1995 ,1999 ,2004) .… 相似文献
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新编制的地震动参数区划图采用了潜在震源区三级划分方案,以体现背景地震活动空间分布的不均匀性,并在地震构造区内归纳出统一的地震构造模型.本文根据西南地区潜在震源区三级划分的成果,分析了龙门山地震统计区内的龙门山和成都地震构造区的基本特征,历史地震活动强度及频度,主要活动构造的构造变形样式,建立了地震构造区的发震构造模型,确定了构造区的本底地震及划分构造源的地震构造标志.同时,提出了确定背景源空间分布函数的简单方法. 相似文献
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时间相依模型与泊松模型计算结果的对比分析——以道孚及炉霍潜源为例 总被引:1,自引:1,他引:0
本文分析了华北平原第四纪主要构造格局和强震活动特点,划分了主要强震构造带,并对其发震能力作了评价。认为坝县-束鹿-邯郸断裂带、唐山-河间-磁县断裂带和黄骅-德州-东明断裂带3条北东向右旋走滑断裂带为华北平原裂谷系从早第三纪伸展拉张作用进入晚第三纪-第四纪走滑剪切拉张作用的产物,这3条断裂带分别位于3个北东向坳陷带中部,并构成了第四纪沉降中心,与营口-潍坊断裂带一起构成华北平原内的主要强震构造。本文最后提出了华北平原区划分潜在震源区应注意的几点问题,进而针对第四代区划图中华北平原区潜在震源区划分综合方案提出了补充修改意见。 相似文献
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根据地震复发周期模型, 利用现有的地质构造等资料把南北地震带划分为若干相对独立的活动构造区, 对能量积累阶段及地震危险性的预测建立相应的数学模型, 并构建基于WebGIS的网络计算平台, 由客户端任意在研究区选择构造分区, 并输入所选构造分区相应的计算参数, 提交到集群服务器计算模型进行计算, 对所选构造分区的地震危险性阶段及潜在震级进行预测并把结果以WebGIS方式返回给客户端。 实现了利用远程计算技术与并行算法对活动断裂能量积累与释放过程的模拟计算, 其结果可以为判定地震中短期预测的地点和震级提供依据。 相似文献
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地震危险区的边界划分探讨 总被引:1,自引:0,他引:1
本文针对目前地震危险区边界划分上存在的问题,从地震地质和地震构造的角度,结合测震学方法进行了分析,指出地震分布和地震危险区边界划定与活动构造有密切的联系。依据这一思想,阐明了构造活动与地震活动的关系,初步提出了地震危险区边界判析的原则,即把地震危险区限制在一定的地震构造区(带);其边界依据活动构造划定;在地震危险区内部进行发震构造条件研究,并对这些发震构造(活断层)进行活动度分析;分层次地对地震危险区范围及其危险度进行确定。 本文着重进行了活动构造的研究,对中国大陆的活断层、新生代盆地、地形面以及古地震等作了活动时代、活动性质、活动强度等多方面的论述。 相似文献
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This paper reviews the history and progress of research on active tectonics in China and overseas.By giving a brief introduction on the history of active tectonic research in China and other countries,the paper sums up the process and development of quantitative investigation of active tectonics since the 1980s.The focus is on the main efforts and progress made in China on certain aspects of research,such as basic surveys and applied investigation of active tectonics,the study of theories related to regional active tectonics and their kinematics and geodynamics,surveys on coupling relations between deep and shallow structures,active fault surveys and prospecting and seismic hazard assessment in urban areas,as well as the efforts made using Quaternary geochronology.Furthermore,the paper looks back on Chinese quantitative investigation of active tectonics in China and sums up cognitions derived from studies on the determination of several basic and measurable parameters of active tectonics.These parameters include the length of fault and fault segmentation,coseismic slip and cumulative slip,fault slip rate,the sequence of paleoearthquake events and the time elapsed since the most recent event.At the same time,efforts and progress made in China on assessing the long-term seismic potential for active faults and evaluating the risk from potential active fault movement have been reviewed by summarizing research on developing theories,models,methods and the application of time-dependent seismic potential to probabilistic assessment,magnitude estimation for potential earthquakes on active faults,and the forecast of potential risk caused by active fault movement.Finally,in consideration of the realities and problems in the research of active tectonics in China,the authors put forward several suggestions for issues worthy of more attention for further investigation in the future. 相似文献
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This paper reviews the history and progress of research on active tectonics in China and overseas. By giving a brief introduction on the history of active tectonic research in China and other countries, the paper sums up the process and development of quantitative investigation of active tectonics since the 1980s. The focus is on the main efforts and progress made in China on certain aspects of research, such as basic surveys and applied investigation of active tectonics, the study of theories related to regional active tectonics and their kinematics and geodynamics, surveys on coupling relations between deep and shallow structures, active fault surveys and prospecting and seismic hazard assessment in urban areas, as well as the efforts made using Quaternary geochronology. Furthermore, the paper looks back on Chinese quantitative investigation of active tectonics in China and sums up cognitions derived from studies on the determination of several basic and measurable parameters of active tectonics. These parameters include the length of fault and fault segmentation, coseismic slip and cumulative slip, fault slip rate, the sequence of paleoearthquake events and the time elapsed since the most recent event. At the same time, efforts and progress made in China on assessing the long-term seismic potential for active faults and evaluating the risk from potential active fault movement have been reviewed by summarizing research on developing theories, models, methods and the application of time-dependent seismic potential to prohabilistic assessment, magnitude estimation for potential earthquakes on active faults, and the forecast of potential risk caused by active fault movement. Finally, in consideration of the realities and problems in the research of active tectonics in China, the authors put forward several suggestions for issues worthy of more attention for further investigation in the future. 相似文献
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Basic characteristics of active tectonics of China 总被引:84,自引:8,他引:76
Active tectonics is inferred to all the structures which have been active since the late Pleisto-cene, 100—120 ka B.P., are still active recently, and will be active in a certain time period in the future, such as active faults, active folds, active basi… 相似文献