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1)  seismic condition which induce earthquake
诱发地震条件
2)  Inducing earthquake condition
诱震条件
1.
The inducing earthquake conditions such as the seismicity, stress state,karst and permeability of rock in the reservoir are analyzed , and the maximum magnitude and .
采用断层强度分析法分别估算了小浪底水库蓄水前和一些断层面的抗滑稳定系数 ,对库区地震活动性、应力状态、岩溶和岩体渗透性等诱震条件进行了分析。
2.
The inducing earthquake conditions of the Qiaoqi and Zhonggang Reservoir are comprehensively analyzed according to the field investigation, and it is compared with other reservoir.
根据野外实地考察 ,对硗碛、中岗水电工程水库诱发地震的诱震条件进行了综合分析 ,并与其它水库的发震条件进行对比 ,对该两水库诱发地震的可能性作出了初步评价 ,并对可能发震的地段、最高震级和烈度以及对工程的影响进行了估
3)  induced earthquake
诱发地震
1.
Mechanism of reservoir-induced earthquake and earthquake resistant fortification;
水库诱发地震机制与抗震设防
2.
Prediction of the reservoir induced earthquakes in the Ertan Hydropower Station;
二滩水电站水库诱发地震预测
4)  induced seismicity
诱发地震
1.
So it is necessary to establish the database of Danjiangkou reservoir induced seismicity which will be applied to the prediction of seismicity,the quakeproof and redu.
所以,有必要对丹江口水库诱发地震数据建立基础数据库,为水库续建工程的地震预测,库区的防灾和减灾服务。
2.
So estimating the magnitude of reservoir induced seismicity is profound to the quakeproof and reducing disaster of reservoir area.
进行丹江口水库二期工程诱发地震危险性分析和预测震级对水库的防灾和减灾具有十分重要的意义。
5)  induced earthquakes
诱发地震
1.
A brief introduction of fundamental and applied researches in the field of seismology engaged by the seismological division under KNMI has been given in the paper, the researches are focused on infrasound, induced earthquakes, mining law and the projects in the European centre for exchange and coordination of seismological data (ORFEUS) hosted by the seismological division.
简要介绍了荷兰皇家气象研究所(KNMI)地震部所进行的地震领域的基础和应用性研究,其中包括次声研究、诱发地震研究、采矿法以及地震部所主持的欧洲地震数据交换和协调中心的工作。
2.
The prediction ability of induced earthquakes is tested from statistical simulation.
用诱发地震的方法研究了 1 970年 1月 1日至 1 998年 1 2月 31日华北地区发生的 A-F- B震的关系 ,以及诱发地震的空间分布特征。
3.
The induced earthquakes happened near the well, the magnitudes of these earthquakes are small, the earthquake sources are shallow, and they belong to the main shock after shocktype or the swarmtype earthquakes, but not belong to the solitary type earthquakes.
通过对国内外众多震例的分析 ,发现了向深井抽 (注 )水 (液体 )诱发地震的一些普遍规律 :诱发地震的震中在井位附近 ,震级小 ,震源浅且多为主余震型或震群型 ,绝少有孤立型地震发生 ;诱发地震的多少和大小与抽 (注 )水的压力和数量相关 ;诱发地震一般在钻井时注入泥浆、洗井时注入高压清水或正常的地下水开采等 3种情况时马上发生 ,或滞后 1~ 2 0天发生 。
6)  induced conditions
诱发条件
补充资料:水库诱发地震
      见诱发地震。
  

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