2014年于田M_S7.3地震对后续余震和远场小震活动的动态应力触发          下载免费PDF全文

王琼  解朝娣  冀战波  刘建明 《地球物理学报》2016,59(4):1383-1393

本文采用离散波数法,计算了2014年于田M_S7.3地震的断层破裂在近场和远场产生的库仑破裂应力变化,并结合地震活动特征,讨论了M_S7.3地震对后续余震活动和远场区域小震活动的动态应力触发作用.结果表明, ① M_S7.3地震产生的库仑破裂应力变化对其西南侧主体余震区的地震活动起到了抑制作用,这可能是本次M_S7.3地震序列余震活动水平不高的主要原因;距主震约30 km的北东方向余震区后续地震活动受到了主震产生的动态和静态应力变化的共同触发作用,动态应力变化峰值为2.78 MPa,静态应力变化为0.80 MPa,这与该区余震较为活跃相一致;距主震约45 km的北部余震区受到动态应力触发作用,应力变化峰值为0.72 MPa. ② M_S7.3地震产生的动态库仑应力变化空间分布呈非对称性,其中北东方向、北部余震分布与动态应力变化正值区存在相关性,从应力变化的角度解释了M_S7.3地震的后续余震空间活动特征. ③ M_S7.3地震在沙雅、伽师地区的远场接收点产生的动态应力变化峰值分别为0.09 MPa、0.1 MPa,对两个区域的小震活动具有动态触发作用.  相似文献   

基于LXI总线的接口转换器的设计     

孙大雷  王天宝 《成都信息工程学院学报》2008,23(1):8-11

LXI是安捷伦公司和VXI科技公司联合提出的一种新型仪器接口规范,它最大的特点是基于以太网技术,可满足于组建网络化测试系统,是新一代总线标准的代表。介绍了LXI总线的产生以及技术特点,提出一种基于LXI总线协议的接口转换器的设计方案,详细说明了硬件的设计、触发方式的选择、接口驱动及模块间的通信。  相似文献   

Stress triggering of normal aftershocks due to strike slip earthquakes in compressive regime   总被引：2，自引：0，他引：2  

Kalpna Gahalaut  V.K. Gahalaut   《Journal of Asian Earth Sciences》2008,33(5-6):379-382

A few cases of occurrence of normal aftershocks after strike slip earthquakes in compressive regime have been reported in the literature. Occurrence of such aftershocks is intriguing as they occurred despite the apparent stabilizing influence of compressive plate tectonic stresses on the normal faults. To investigate the occurrence processes of such earthquakes, we calculate change in static stress on optimally oriented normal and reverse faults in the dilational and compressional step over zones, respectively, due to slip on a vertical strike slip fault under compressive regime. We find that change in static stress is much more pronounced on normal faults as compared to that on reverse faults, for all values of fault friction. Change in static stress on reverse fault is marginally positive only when the fault friction is low, whereas for normal faults it is positive for all values of fault friction, and is maximum for high fault friction. We suggest that strike slip faulting in compressive regime creates a localized tensile environment in the dilational step over zone, which causes normal faulting in that region. The aftershocks on such normal faults are considered to have occurred as an almost instantaneous response of stress transfer due to strike slip motion.  相似文献   

A Review of Research on Warm-Sector Heavy Rainfall in China     

Jianhua SUN  Yuanchun ZHANG  Ruixin LIU  Shenming FU  Fuyou TIAN 《大气科学进展》2019,36(12):1299-1307

  相似文献   

Lunar and solar tidal components in the occurrence of earthquakes in Italy   总被引：2，自引：0，他引：2  

A. Palumbo 《Geophysical Journal International》1986,84(1):93-99

Summary. A method for the determination of lunar and solar daily components of earthquakes is proposed. Its application to the most intense earthquakes with epicentres in Italy (from 1900 to 1983) provides for the first time large and significant lunar and solar tidal terms. The absence of significant results from the analysis of 9157 world-wide large shocks processed according to the proposed method and to routine spherical harmonic techniques indicates that the Italian earthquakes are locally tidally triggered.  相似文献   

地壳中的应力场及一些诱震因素     

曾心传 《大地测量与地球动力学》1997,(1)

把地球考虑为在径向上由ｎ层具有不同物理—力学性质的物质所组成的球体，由此出发，推导了计算地壳中由地球自重、匀速自转、天体引力、地球自转速度变化所产生的位移场和应力场的公式。对由地壳和地幔以下物质所组成的二层体情形进行了详细推演，数值计算表明：作为诱震因素，天体引力特别是月亮对地球的引力似乎比地球自转速度变化所起的作用更大  相似文献   

2个二次触发型太阳耀斑的射电时间轮廓及其日冕磁结构     

谢瑞祥  郝龙飞  颜毅华  许春  刘玉英  施硕彪  李维华 《天文研究与技术》2006,3(3):247-257

利用国家天文台(北京和昆明)的射电频谱仪(频段为0.65~7.6 GHz)和相关的NoRH/17GHz射电以及TRACE/171 EUV和Yohkoh/SXT的观测资料,分析了2001/04/10和10/19的2个共生精细时间结构的稀有事件,这2个事件的射电爆发时间轮廓和观测特征相似,通过这2个事件的微波(17GHz)偏振观测资料的比较,发现这2个射电爆发均由包含多重(4极)磁结构的复杂活动区引起,特别指出这2个耀斑最后都导致了耀斑后相的分米波射电爆发(第二次触发耀斑),这可能是后环引起的射电爆发。它们都分别对应于双极磁位形,表明这两次触发耀斑是由相似的耀斑模型产生。2个分米波爆发可能是相似(homologous)耀斑的射电表现,可以推测这两次耀斑的驱动器可能皆是磁流浮现或对消(因为源区有新的单或双极出现或消失),而它们的触发器皆是由双极反向Y型位形(具有一个双极拱的单磁流系统)的磁重联,耀斑后环的演化是导致耀斑后相分米波射电爆发的必要条件。我们认为,这双带耀斑对应的宽带射电爆发辐射机制是回旋同步加速辐射过程,而耀斑后相的窄带分米波爆发的辐射机制是等离子体辐射过程。  相似文献   

中国及邻区地震的天文潮汐触发特征研究——附加潮汐应力对发震断层的作用模式及其应用     

吴小平 《天文研究与技术》2002,(1)

本文在潮汐应力、构造应力、地震断层和岩石破裂滑动理论的基础上 ,建立了潮汐应力对地震断层作用的力学模式 ,该模式将潮汐应力与地震应力作用相结合 ,描述了沿地震主压应力和地震主张应力方向的附加潮汐应力对发震断层的力学作用方式 ,从而切入潮汐应力触发地震的物理机制 ,认为潮汐对地震的触发作用在实质上归结为潮汐应力对地震断层的促滑作用 ,这种促滑作用分增压型和减压型。在此模式基础上 ,对中国大陆及邻区的不同类型地震的潮汐触发性进行了研究 ,内容包括 :计算了中国及邻区一千多个地震震源处沿主压应力P轴和主张应力T轴方向的附加潮汐应力分量 ,分析了这些量对发震断层的作用方式 ,按纬度区域统计了受到潮汐应力促滑作用的发震断层类型以及它们与潮汐应力作用方式的关系 ,得到了如下结论 :受到潮汐应力促滑作用的发震断层的比例随区域纬度增加有减小趋势 ,其中 ,走滑型断层的比例在低纬区较大 ,而倾滑斜型断层的比例在中高纬度区较大 ;对整个统计区域而言 ,受增压型潮汐应力促滑作用的发震断层数比例大于受减压型潮汐应力促滑作用的发震断层 ;对不同的纬度区域 ,不同的潮汐应力作用方式与之促滑的发震断层类型也有不同的分布特征。最后 ,本文将中国及邻区受到潮汐触发作用的地震按构造应力  相似文献   

Sources of uncertainty in liquefaction triggering procedures     

John T. Christian  Gregory B. Baecher 《Georisk: Assessment and Management of Risk for Engineered Systems and Geohazards》2016,10(4):242-250

Uncertainties in observed data and in processing field and laboratory tests are major concerns. Assigning reasonable coefficients of variation to the parameters in the conventional analyses indicates that a site with deterministic factors of safety of 1.5 can actually have liquefaction triggering probability above 20%. About a third of the variance comes from uncertainty in the load, which is independent of the resistance. Researchers have traditionally presented the results of case studies in the form of charts showing instances in which liquefaction did and did not occur and have developed relations to separate the two. Although the original researchers developed the separations informally, recent work has applied statistical methods. These give the sampling distributions of the observed data rather than the probability of triggering given the data. Researchers have addressed this issue using Bayesian methods, adopting non-informative priors. Published curves of liquefaction probabilities can be interpreted as likelihood ratios. Other independent work demonstrates that geological, meteorological, and historical data can be used to develop prior probabilities, so it may not be necessary to assume a non-informative prior. The actual prior can then be combined with the likelihood ratios to provide rational probabilities of liquefaction. We recommend that researchers publish their likelihood ratios and allow engineers faced with particular sites to use those to update their own priors.  相似文献   

广州夏茅村岩溶塌陷灾害特征及防治对策     

易顺民  卢薇  周心经 《热带地理》2021,41(4):801-811

通过对广州夏茅村岩溶塌陷进行地质勘察,系统探讨了当地的地质环境条件、岩溶塌陷的灾害特征、岩溶发育条件和岩溶塌陷的形成原因。结果表明,区内第四系覆盖土层厚度大且分布不均,土洞大量发育,隐伏可溶岩的富水性好,溶洞发育;同时,覆盖层内的松散岩类孔隙水与下伏灰岩裂隙溶洞水之间的水力联系密切,含水砂层内地下水位的改变会直接引起下伏灰岩裂隙溶洞水的水位波动,构成岩溶塌陷的水动力因素;钻孔桩施工时钻孔揭穿覆盖层内土洞顶部的黏性土层盖板,造成盖板上部的细砂及淤泥流入土洞,是岩溶塌陷的直接触发因素。在此基础上,提出建立岩溶分布区的地下水动态长期监测网,对岩溶塌陷地段进行灌浆处理,是根治夏茅村岩溶塌陷的主要有效途径。  相似文献