地震带

dì zhèn dài
  • seismic belt;earthquake zone
地震带地震带
地震带 [dì zhèn dài]
  • [seismic belt;earthquake belt] 地震震中分布较集中的地带

  1. 利用GIS方法研究南北地震带和中央造山带交汇区活动断裂与地震的关系

    A GIS Research on the Relationship Between Active Faults and Earthquakes in China North-south Seismic Belt and Central Orogenic System Intersection Zone

  2. GM模型在南北地震带中南段地区强地震序列预测中的应用

    The Application of GM Model To Predicting Strong Earthquake Sequences In the Region of Middle and Southern Segments of South-north Seismic Belt

  3. 日本是一个位于地震带上的国家,它非常善于应对地震。

    Japan is a country which lies on the earthquake beltand it is very good at dealing with earthquakes .

  4. 汾渭地震带的b值和年平均发生率的研究

    Study on b Value and Average Annual Incidence of Earthquakes in Fen-wei Seismotectonic Zone

  5. 中国南北地震带北段分层地壳速度结构模型的二维CT成象电磁波井间CT成象技术及其在岩土工程中的应用

    Two Dimension C F Imaging of Northern section Earth-crust Layer Velocity Constructure of South-north Seismic Belts in China

  6. 震级加权四指标Blade算法及在地震带识别中的应用

    The Ms-weighted 4-index blade algorithm and its application for identifying the seismic belts in the Great North China

  7. 本文对燕山地震带近30年来的地震活动参数E、N、E~(1/2)和b值进行了系统的分析。

    This paper systematically analyzed the seismicity parameters , E , N , E and b values in almost 30 years in the Yanshan seismic zone .

  8. 使用全球定位系统(GPS)卫星接收仪在美国新马德里地震带重新测量了历史上的三角网,并据此估算了震间应变速率。

    Results of interseismic strain rate determined by re-occupation of a historical triangulation network in the New Madrid seismic zone by the Global Position System ( GPS ) are reported .

  9. 在南北地震带中、南段(98°~105°E,21°~34°N)可划分成7个小区。

    The middle south part ( 98 ° ~ 106 ° E , 21 ° ~ 34 ° N ) of South North seismic zone can be zoned into seven small areas .

  10. 应用川滇11个地震带(区)资料,研究了与地震频度N或地震能量E有关的各种地震学指标在描述地震活动性变化方面的相关性。

    Correlation among various seismological prediction indexes related to earthquake frequency N or energy E for describing seismicity changes is studied by seismic data of 11 seismic zones ( areas ) in the Sichuan Yunnan region .

  11. 本文用韦布尔(Weibull)分布对陕西省及汾渭地震带的中强地震活动进行概率统计分析,得到所研究地区的中强地震平均复发周期和发震概率。

    In this paper , the average recurrence period and probability of moderately strong earthquake in shaanxi province and Fen & Wei seismic belt are obtained using Weibull distribution .

  12. 本文以汾渭地震带为例和以小震P、S振幅比测定的震源参数尝试应用了用小震断层面解反演区域平均应力场的方法。

    In this paper , taking the Fen & wei seismic belt for example , and using the amplitude ratio of P 、 S to determine the seismic source parameters , it was inversed regional mean stress field by using the fault planes of small earthquake .

  13. 此种布局将避开台湾和菲律宾之间的吕宋海峡(LuzonStrait)地震带,在该地区近期的地震中,此处的光缆遭到了损坏。

    This configuration will avoid the Luzon Strait seismic zone between Taiwan and the Philippines , where the cables damaged by the recent earthquake were located .

  14. 通过对南北带1999~2001、2001~2004年GPS资料的处理与分析,结果显示:南北地震带是我国水平运动的转化带与形变带;

    The GPS measurement data 1999 ~ 2001 and 2001 ~ 2004 observed along the North-South Seismic Belts are processed and analyzed . Our results show that the North-South Seismic Belts are the transfer belts of horizontal movements and deformation .

  15. 利用灰色系统理论中的GM(1,1)灾变预测模型,建立了北天山地震带强震(M≥6.5)的预测模型。

    Using GM ( 1 . 1 ) catastrophic model of grey system theory , a predictive model of strong earthquake ( M ≥ 6 . 5 ) in North Tianshan seismic area has been set up .

  16. 本文选择地壳形变观测资料较丰富而又备受关注的燕山渤海地震带,首先利用GPS区域网复测资料研究燕山渤海带的相对运动与变形方式、应变积累背景及其分段特征等。

    We focus on Yanshan bohai seismic zone in this paper , in which there are plentiful crustal deformation observations . Firstly , we studied the relative motion and mode of texturing , strain accumulation and its sub-features of Yanshan Bohai Zone by processing the GPS velocity data .

  17. 在自东向西各地震带的活动能量急剧下降的同时,相应的地热流异常值有一个上升趋势,海峡西岸的地热异常高值多分布在NE与NW向断裂的交汇点上。

    From east to west , the energy liberation of each seismic zone decreases abruptly , but the value of geothermal anomalies increases . The high value of geothermal anomalies west of the Taiwan Strait basically appears at the intersection between the NE-trending fault and the NW-trending fault .

  18. 作为对中东亚塑性流动网络系统平均状况的估计,网带的热异常宽度与地震带所显示的网带视宽度一致,约为65km;

    It is indicated as an estimation of the average situation for the Central-Eastern Asia ( CEAs ) plastic-flow network system that the thermal-anomaly width of PFB is identical with the average apparent-width of PFBs manifested by seismic belts , being approximate to 65km ;

  19. 南北地震带强震复发间隔的估计

    Estimation of recurrent interval of strong earthquakes in NS earthquake belt

  20. 板缘构造作用对泉州&汕头地震带的影响

    Influence of the marginal plate tectonism on the quanzhou-shantou seismic zone

  21. 南北地震带北段硅热流值

    Silica heat flow in the northern segment of North-South Seismic Belt

  22. 北天山地震带的航磁异常与深部构造

    Aeromagnetic anomaly and deep tectonics in the Northern Tianshan seismic belt

  23. 北天山地震带的强震活动特征

    Characteristics of seismicity of strong earthquakes in North Tianshan seismic zone

  24. 山东中部一条明显的北西向中强地震带

    An evident NW-trending seismic zone of medium-strong earthquake in central Shandong Province

  25. 利用前兆事件对新马德里地震带进行中期地震预测

    Intermediate-term earthquake prediction using precursory events in the New Madrid seismic zone

  26. 山西地震带热流体对强震活动的影响

    The influence of hydrothermal body on strong earthquake activity along

  27. 亚欧地震带仍保持非常平静的状态。

    The Eurasian seismic belt still re - mained in extreme quiescence .

  28. 建立了南北地震带北段下地壳部分熔融几何形状和分布的模型。

    Partial melt models in different geometrical configuration and distribution are established .

  29. 汾渭地震带地震发生的统计分析

    Statistical analysis on the earthquake occurrence in FEN-WEI seismic zone

  30. 山西地震带地震危险性研究

    A Study on the Hazardousness of Earthquakes in Shanxi Belt