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earthquake region
相关语句
  震区
    Study on Crust Structure of Haiyuan Strong Earthquake Region
    海原8.5级大震区地壳结构探测研究
短句来源
    The application of Wavelet Transform to the process of water level observational data for weak earthquake region
    小波变换在少震、弱震区地下水位数据分析中的应用
短句来源
    DIFFERENCES OF CRUSTAL STRUCTURES IN NORTHEASTERN EDGE OF TIBET PLATEAU, ORDOS AND TANGSHAN EARTHQUAKE REGION IN NORTH CHINA-RESULTS OF DEEP SEISMIC SOUNDING
    青藏高原东北缘、鄂尔多斯和华北唐山震区的地壳结构差异——深地震测深的结果
短句来源
    STRONG GROUND MOTION AT MEIZOSEISMAL AREA & SAFETY OF IMPORTANT ENGINEERING PROJECTS AT POTENTIAL EARTHQUAKE REGION
    极震区的地震动与潜在震源区内重大工程安全
短句来源
    It takes earthquakes with Ms≥5.5 in Minor North China and those with Ms≥4.5 in Tangshan earthquake region for example analyses.
    对小华北地区M_S>≥5.5地震,唐山老震区M_S≥4.5地震进行了震例分析。
短句来源
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  地震区
    The seismicity of the studying area (29°~35°N, 114°~120°E), which is located in the transition area of earthquake region in North China and South China, is not high, and the attenuation of intensity has its own characters in focal mechanism, radiate medium and site.
    研究区(北纬29°~35°,东经114°~120°)位于华北地震区和华南地震区之间的过渡地区,地震活动性总体水平不高,烈度衰减关系有其自身的震源特性、传播介质和场地衰减特性等。
短句来源
    At present,the principal compressive strain rate in Xingtai earthquake region is very small,with a magnitude of-0.352×10~(-9)/yr,and the principal tensile strain rate is relatively large,with a magnitude of 3.306×10~(-9)/yr,which shows that the tensile strain in this area is predominated,and the crust is in a tensional state;
    当前,邢台地震区主压应变率很小为-0.352×10-9/yr,主张应变率较大为3.306×10-9/yr,张应变占绝对优势,地壳处于拉张状态;
短句来源
    in Bohai earthquake region,the principal compressive strain rate is-2.593×10~(-9)/yr,which is a little bit smaller than the tensile strain rate(2.947×10~(-9)/yr);
    在渤海地震区,主压应变率为2.593×10-9/yr,比主张应变率(2.947×10-9/yr)略小一些,二者比较接近;
短句来源
    in Haicheng earthquake region,the principal compressive strain rate(1.276×10~(-9)/yr) is smaller than the tensile strain rate(2.940×10~(-9)/yr),where is dominated by tensile strain;
    在海城地震区,主压应变率为1.276×10-9/yr,小于主张应变率(2.940×10-9/yr),地壳以张应变为主;
短句来源
    A PRELIMINARY STUDY ON FINE STRUCTURES OFJIASHI EARTHQUAKE REGION AND EARTHQUAKEGENERATING FAULT
    伽师地震区地壳细结构及发震断层的初步研究
短句来源
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  震源区
    Study on the Geological Structural Criteria on Determination of Potential Earthquake Region
    划分潜在震源区的地震地质规则研究
短句来源
    STRONG GROUND MOTION AT MEIZOSEISMAL AREA & SAFETY OF IMPORTANT ENGINEERING PROJECTS AT POTENTIAL EARTHQUAKE REGION
    极震区的地震动与潜在震源区内重大工程安全
短句来源
    The main characteristics of seismic activity before M_S6 earthquakes are the M_S4 seismic activity pass intensity-quietude course in the same tectonics under intensity background of different periods,the seismic activity are different in the earthquake region 3 months before M_S6 earthquakes in different tectonics.
    ②新疆发生6级地震的主要地震活动特征是,在不同时段的增强背景下,构造带4级地震活动经历增强—平静过程,不同构造区震前3个月震源区的活动具有各自的特点;
短句来源
    Main Tendency of the Study on the Potential Earthquake Region at Present
    当前潜在震源区研究的主要方向
短句来源
    Determination of Potential Earthquake Region with Artificial Neural Network
    应用人工神经网络划分潜在震源区
短句来源
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  “earthquake region”译为未确定词的双语例句
    Velocity structure of the crust and upper mantle in Xingtai earthquake region andits adjacent area
    Velocity structure of the crust and upper mantle in Xingtai earthquake region and its adjacent area
短句来源
    Monitoring ability of Fujian digital seismic network to the historical strong earthquake region of Quanzhou
    福建数字地震台网对泉州地震的监测能力
短句来源
    PASSIVE SEISMIC EXPERIMENT IN XINGJIANGJIASHI STRONG EARTHQUAKE REGION AND DISCUSSION ON ITS SEISMIC GENESIS
    新疆伽师强震群区三维地壳上地幔S波速度结构及其地震成因的探讨
短句来源
    FEATURES OF THE S-WAVE SPLITTING AND STRESS FIELDIN THE XINJIANG JIASHI STRONG EARTHQUAKE REGION
    新疆伽师强震群区的横波分裂与应力场特征
短句来源
    Data Processing of Nearfield Earthquake Records in Jiashi Earthquake Region——3-D Velocity Tomograthy
    伽师近场地震资料处理——三维速度成像
短句来源
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  earthquake region
Seismicity in the Vogtland/Western Bohemia Earthquake Region Between 1962 and 1998
      
A peculiarity of the Vogtland/West Bohemia earthquake region is the appearance of earthquake swarms.
      
Probabilistic assessment of earthquake recurrence in the January 26, 2001 earthquake region of Gujrat, India
      
Deep electrical anomaly in the M7.5 Qiongzhou earthquake region and its relation with future seismicity
      
Three-dimensionalQ structure in Jiashi earthquake region of Xinjiang
      
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The paper introduced the field recording system for the data of deep seismic sounding completed on STM-PC microcomputer series, including the A/D conversion and data acguisition for the seismic recordings of analog tapes. Through the study of time-scale singnal acquisition, six-sound singnal proceeding, analog plagback circuite improvement and acquisition rates, etc. the experience of conducting A/D conversions with high quality is obtained. Upon statistical data the precision is analysed on the basis of practical...

The paper introduced the field recording system for the data of deep seismic sounding completed on STM-PC microcomputer series, including the A/D conversion and data acguisition for the seismic recordings of analog tapes. Through the study of time-scale singnal acquisition, six-sound singnal proceeding, analog plagback circuite improvement and acquisition rates, etc. the experience of conducting A/D conversions with high quality is obtained. Upon statistical data the precision is analysed on the basis of practical data of the Haicheng earthquake region, the research results show that the A/D conversion precision for analog seismic record of this system conforms to the standard, and this system compatible with usual microcomputers will suit the tape recorders to be used in our country.

本文介绍了STM-PC微机系列上实现的地震测深资料现场收录系统,其中包括对模拟磁带地震记录进行A/D转换、数据采集等。在研究中,对时标信号的采集方式、六响报时信号处理、模拟回放电路的改进与采集速率等方面进行了试验,为高质量地进行A/D转换取得了经验。本文是以海城震区的实际资料为基础,对A/D转换的精度与效果进行了统计与分析,结果表明,该收录系统对模拟地震记录的A/D转换精度达到了规范要求。该收录系统与一般微机系列兼容,适用于我国目前使用的几种模拟磁带地震记录仪。

The typical earthquake disaster and its seismogenic mechanism in the meizoseismal regions of M7. 6 Lancangand M7. 2 Gengma earthquakes are introduced and analysed in this paper. Combining with the tectonic features in the earthquake regions, the difference of the tectonic activity between the two earthquakes is alsoshown in the paper: the strong strike offset feature of Muga fault for M7. 6 Lancang earthquake, while thedip-slip feature of Hanmuba fault for M7. 2 Gengma earthquake....

The typical earthquake disaster and its seismogenic mechanism in the meizoseismal regions of M7. 6 Lancangand M7. 2 Gengma earthquakes are introduced and analysed in this paper. Combining with the tectonic features in the earthquake regions, the difference of the tectonic activity between the two earthquakes is alsoshown in the paper: the strong strike offset feature of Muga fault for M7. 6 Lancang earthquake, while thedip-slip feature of Hanmuba fault for M7. 2 Gengma earthquake. The obvious difference in the displacementbetween Muga fault and Hanmuba fault probably related to the part adjustment and diversion for the principalcompressive stress axis in the focal area of M7. 2 Gengma earthquake. The M7. 6 Lancang earthquake triggered M7. 2 Gengma earthquake.

Seismogenic mechanism of the Lancang and Gengma earthquakes(俞维贤)(周瑞琦)(候学英)(周光全)SeismogenicmechanismoftheLancangandGengmaearth...

In terms of inversion method and programme for frequency- domain magnetization intensity, airborne magnetic data from the Tangshan- Luanxian earthquake region are processed and the horizontal distribution of apparent magnetization intensity in this region is obtained. The inversion results reflect the project of the crustal rock masses with different scale and magnetism on plane in the earthquake region. With combination of time-space distribution and fracture direction of the earthquakes...

In terms of inversion method and programme for frequency- domain magnetization intensity, airborne magnetic data from the Tangshan- Luanxian earthquake region are processed and the horizontal distribution of apparent magnetization intensity in this region is obtained. The inversion results reflect the project of the crustal rock masses with different scale and magnetism on plane in the earthquake region. With combination of time-space distribution and fracture direction of the earthquakes in the Tangshan-Luanxian region, seismogenic process in this region is approached in the paper.

依据频率域磁化强度反演方法和程序,对唐山滦县震区航磁资料进行了数据处理,求取了该区视磁化强度的水平分布。反演结果反映了震区地壳内不同规模、不同物性的地壳岩体在平面上的投影。本文结合唐山滦县震区地震的时空分布及破裂方向,对该区地震的孕育及发生过程进行了探讨。

 
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