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地震类型

地震类型的相关文献在1989年到2021年内共计68篇,主要集中在地球物理学、信息与知识传播、中国政治 等领域,其中期刊论文65篇、会议论文3篇、专利文献30866篇;相关期刊34种,包括地震、地震学报、大地测量与地球动力学等; 相关会议3种,包括第八届全国地震工程会议、中国地震学会成立三十年学术研讨会、中国地质学会地质学史专业委员会第20届学术年会等;地震类型的相关文献由158位作者贡献,包括秦嘉政、刘蒲雄、曲延军等。

地震类型—发文量

期刊论文>

论文:65 占比:0.21%

会议论文>

论文:3 占比:0.01%

专利文献>

论文:30866 占比:99.78%

总计:30934篇

地震类型—发文趋势图

地震类型

-研究学者

  • 秦嘉政
  • 刘蒲雄
  • 曲延军
  • 李忠华
  • 王强
  • 皇甫岗
  • 邬成栋
  • 陈修启
  • 于江
  • 兰从欣
  • 期刊论文
  • 会议论文
  • 专利文献

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    • 康莉莉; 刘名吉; 张洪博; 杨青松
    • 摘要: 基于日本KiK-Net、K-Net地震台网和太平洋地震工程中心(PEER)的14713条地震动记录,比较了俯冲带地区浅壳上地幔地震、板内地震和板间地震的水平向地震动加速度反应谱阻尼修正系数(DMF)和位移反应谱阻尼修正系数(DMF)的差异,并进行了5%置信水平下的假设检验,探究了俯冲带地区不同地震类型对DMF的影响。结果显示:在大多数谱周期,不同地震类型的DMF存在统计意义上的显著差异;在低阻尼比中短周期时,加速度谱DMF和位移谱DMF基本相同;在高阻尼比长周期时,不同地震类型的加速度谱DMF差异大于位移谱DMF差异。研究表明:俯冲带地震水平向地震动DMF需要考虑不同地震类型的影响。
    • 温超; 蔡玲玲; 黎勇; 孟立朋; 周月玲; 张合; 郭秋娜
    • 摘要: 系统地整理和分析了河北省有史以来4级以上的地震序列类型,并结合该地区地震地质构造特征进行研究.结果 表明:①河北省地震序列类型以主余型为主,孤立型地震次之;②地震序列类型在空间分布上也有着较为明显的区域特征;③河北省有记载以来M≥4.0地震共计328次,其中有287次地震可确定地震类型,结合区域构造特征,可以将河北省划分为7个不同的地震类型分区,为震后河北省地震序列早期趋势判定提供重要参考依据.
    • 白仙富; 戴雨芡
    • 摘要: 本文收集了1976-2017年滇缅活动地块98个MW 4.8-7.0地震的震源机制解,分析震源机制解和震源深度的空间分布特征,探讨了其构造动力学背景.结果表明:①滇缅活动地块震源深度优势分布范围为10-30km,90%以上的地震震源深度小于30km,结合研究区统计时段内地震震源深度、优势度、众数等参数,推断滇缅活动地块及周边震源深度的下界为30km,脆性多震层位于10-30km,且主要位于15km附近;②滇缅活动块体不同断裂带、块体内部各次级块体之间、块体内外表现出不同的震源机制解,在空间上存在着明显的分区性特征,揭示出位于青藏高原东南缘的滇缅活动块体及周边地区应力场的非均匀性;③滇缅活动地块区域构造应力场明显受周边板块作用的控制,活动地块内部由于构造格局及其运动的差异,应力状态具有明显的区域特征.根据研究区各主要断裂带所反映的与构造背景作用一致的震源机制分布特征,可以将滇缅活动地块初步分为3个应力区.%In this study, focal mechanism solutions for 98 earthquakes MW 4.8-MW 7.0 the in Yunnan-Myanmar active block in last 41 years were collected. We analyzed the focal mechanism solution and the spatial distribution characteristics of focal depth, and discussed related tectonic dynamics. The results are: ①The dominance range of seismic depth is 10-30 km. More than 90% of the earthquake depth is less than 30 km. According to the range, dominance, and mass of seismic depth in the statistical period of our study area, we infer that the bottom of seismic depth locates at 30 km. The brittle seismogenic layer is situated between 10-30 km and mainly located near 15 km.②The spatial distribution of focal mechanism solutions in the study area has obvious regionalization characteristics.This reveals the inhomogeneity of stress fields in the Yunnan-Myanmar active blocks and surrounding areas. ③The regional tectonic stress field of the Yunnan-Myanmar active block is obviously affected by the action of surrounding plates. Due to the difference of tectonic patterns and movements, the stress system has obvious regional characteristics. According to the distribution characteristics of the focal mechanism, which are consistent with the tectonic, the stress division of the Yunnan-Myanmar active block can be divided into 3 parts.
    • 沃梓颖1
    • 摘要: 2016年的夏天,在土耳其的内海马尔马拉海东部,发生了一场5.8级的大地震。这不足为奇,毕竟该地区在过去曾多次发生强烈的地震。问题是,这场地震持续了50天,而且没有一个察觉到它。根据地震学家的说法,这场地震其实属于一种非常奇特的地震类型,被称为“慢地震”。
    • 杨百存; 秦四清; 薛雷; 张珂
    • 摘要: 2017年伊拉克地震发生在我们划分的巴格达地震区,鉴于不同机构提供的该震震级参数相差较大,本文利用孕震断层多锁固段脆性破裂理论,分情况讨论了该震所属地震类型,并分析了巴格达地震区地震趋势.结果表明:若2017年伊拉克地震为Mw7.3,则该震为第3锁固段向峰值强度点演化过程中发生的1次显著前震,该区未来将发生Mw7.7~8.2(双震型为Mw7.5~8.0)标志性地震,目前已接近临界状态;若2017年伊拉克地震为Mw7.5,除可能为显著前震外,还可能为标志性地震(双震)之一,若如此两年内该区将发生另一次Mw7.5地震;若2017年伊拉克地震为Ms7.8,则该震为第3锁固段峰值强度点对应的标志性地震,与我们对该震的前瞻性中长期预测结果相符.我们判断该震不为主震,预测该区未来还将发生MW7.8~8.3(双震型为Mw7.6~8.1)标志性地震,目前该区远离临界状态.%The 2017 Iraq Mw7.3 earthquake occurred in the Baghdad seismic zone defined by us.The seismic type of the earthquake is discussed according to its different magnitude parameters provided by various agencies,and then its post-quake trend in this seismic zone is analyzed in this paper,based on the theory about the brittle failures of multiple locked patches in a seismogenic fault system.The present results show that if the 2017 Iraq earthquake is with a magnitude of Mw7.3,it is identified as a significant foreshock occurred in the evolution process towards the peak strength point of the third locked patch,demonstrating that a Mw7.7~8.2 (or double earthquakes of Mw7.5~8.0) characteristic earthquake will take place in the near future because the seismic zone has closed to the critical state;if the 2017 Iraq earthquake is viewed as Mw7.5,it may yet be one of the double-shock-type characteristic earthquakes besides as a significant foreshock,implying that the other Mw7.5 earthquake will strike the seismic zone within two years;if the 2017 Iraq earthquake is viewed as Ms7.8,it is identified as a characteristic earthquake occurred at the peak strength point of the third locked patch,which is in good agreement with our prospective medium-to-long term prediction of this earthquake.Furthermore,we judge that the Ms7.8 earthquake is not a mainshock,demonstrating that the next Mw7.8~8.3 (or double earthquakes of Mw7.6~8.1) characteristic earthquake will take place in the remote future because the seismic zone is far from the critical state at present.
    • 贾思超; 孙冬军; 毕波
    • 摘要: 随着新型测震软件的开发和新全国一维速度模型的应用,为上海地震监测台网对区域地震的定位精度的提高创造了有利条件.利用JOPENS6.0系统模块内搭载的新型定位方法,对上海及其周边地区所发生的不同震中距、不同类型地震进行重新定位,找出处理各种地震的最优定位方法,从而提高了上海地震台网地震定位精度.研究认为:处理网缘地震时,使用Hypo2000法和自适应演化法定位;处理爆破地震时,选取HypoSAT法及ISCloc法等方法;对于网外地震的处理,建议使用自适应演化法和LocSAT法进行定位;而处理网内近震时单纯型定位法为最合适的选择.
    • 郑旭; 胡进军
    • 摘要: 俯冲带作为陆地板块与海洋板块连接的一个重要区域,其特殊的地理位置决定了在地震研究方面具有重要的意义.为了对俯冲带地震动的特点进行初步了解,本文以日本俯冲带地区为例,通过总结日本俯冲带地震的研究现状,对比分析了该区域俯冲带板内地震、板缘地震以及浅地壳地震的加速度时程、傅里叶谱和反应谱等地震动参数,初步认识了俯冲带地震的特征并为今后关于俯冲带地震的研究打下了理论基础.%Subduction zone is an important area which contacts land and sea plates,the special geographical position determines its importance in earthquake research.In order to know more about the characteristics of earthquake motion in subduction zone,this paper,summaries the research status of subduction zone earthquake in Japan,analyzes the acceleration time history,Fourier spectrum and response spectrum of slab-subduction,interface-subduction and crustal events in Japan,and the characteristics of subduction zone earthquakes are preliminarily recognized,and the theoretical foundation for the study of subduction zone earthquakes is established.
    • 常玉巧; 谢英情; 张彦琪; 李雷; 吴荣帮; 于江; 罗伟东
    • 摘要: We analyzed characteristics of isoseismic lines,earthquake focal mechanism solutions and aftershocks distribution of the Ludian Ms4.9 earthquake.Based on earthquake sequences and focal mechanism solutions,the characteristics of spatial distribution of earthquake type on Zhaotong-Ludian fault zone and its adjacent areas are investigated;Combining the results of field work and previous studies,the seismic tectonic environment is discussed.Main conclusions are drawn as follows:(1) Ludian Ms4.9 earthquake may be related to the activity of the NE-trending Longshu fau(2) Ludian Ms4.9 earthquake may not be a strong aftershock of the Ludian Ms6.5 earthquake occured on August 3,2014;(3) The characteristics of spatial distribution of earthquake type among Zhaotong-Ludian fault zone and its adjacent areas are apparently controlled by the regional faults,which creates a good seimogenic environment.%分析2017年鲁甸Ms4.9地震等震线特征、震源机制解及余震序列特征,从地震序列和震源机制解两方面,分析昭通—鲁甸断裂带及邻区地震类型分布特征;结合野外活动断裂考察成果及前人的研究成果,探讨了昭通—鲁甸断裂带及邻区地震构造环境.初步认为,鲁甸Ms4.9地震可能不是鲁甸Ms6.5地震的强余震.昭通—鲁甸断裂带及邻区地震类型分布受区域断裂控制明显,具有有利的孕震构造环境.
    • 摘要: 前言在地震界,有一个共识,说地震是世界性难题,也就是说地震是不可预测的。那么地震真的是不可预测吗?不!地震是百分之百可以预测的。那么如何才能做到这一步呢?唯一的办法就是利用气象卫星成像(地震)分析技术,如此才能轻易地揭开地震的面纱。
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