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earthquake ability
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  “earthquake ability”译为未确定词的双语例句
     Water Level Change and Reflecting Earthquake Ability of Well No.9-1 of Shanxi
     山西晋_(9—1)井水位变化及映震能力初探
短句来源
     Analysis of Reflecting Earthquake Ability and Anomalies of Mercury in Water of Huailai 4 Well in Hebei
     河北怀来_4井水汞异常及映震能力分析
短句来源
     Analysis of Reflecting Earthquake Ability of Short-Range Leveling in a New Site in Xinyi, Jiangsu
     江苏新沂地震台短水准新场地映震能力分析
短句来源
     Analysis of Reflecting Earthquake Ability of HD-1 Silk Tree Observation System for Earthquake Prediction
     HD-1型合欢树地震观测系统的映震能力分析——以太原基准地震台观测点为例
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     The observational data recorded by FSQ and CZB-1 clinometers are analyzed,and the results are shown that the data quality,the tendency and tide response function of FSQ are better than those of CZB-1,but the reflect earthquake ability of CZB-l is stronger than that of FSQ.
     将兰州台的FSQ与CZB-1仪的观测资料质量、变化趋势、潮汐响应函数及映震能力进行了对比分析,认为:FSQ的观测资料的质量比CZB-1要好,因CZB-1的资料存在漂移现象; 在潮汐因子和相位滞后方面,FSQ比CZB-1反应灵敏;
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  相似匹配句对
     Earthquake
     地震
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     EARTHQUAKE
     日本防震与大地震
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     The Ability of Mirroring Earthquake From Geomagnetic Anomaly
     地磁异常的映震能力
短句来源
     The reflecting and predicting earthquake ability are evaluated.
     对两井的映震效能和地震预报前景进行了评价 .
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     Ability of Sensing
     心动的能力
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Earth-resistivity(ρ_s)changes of Wuwei geoelectric station before and after earthquakes ofM 6.2 in Jingtai county,M 6. 4 in Menyuan,M 4. 7 in West of Tianzhu,M 5. 6 in Danmaand M 4. 7 in Yabulai(Δ≤150 km),as well as M 7. 0 in Gonghe(Δ=270 km) in this paper.Conclusions are follows:( 1)Short-impending ρ_s anomalies up to 10 ̄(-1)─10 ̄(-2) magnitude wererecorded in EW observation direction at the station before the former 4 earthquakes, short-term ρ_s anomalies up to 10 ̄(-2) magnitude which were decreased were recorded...

Earth-resistivity(ρ_s)changes of Wuwei geoelectric station before and after earthquakes ofM 6.2 in Jingtai county,M 6. 4 in Menyuan,M 4. 7 in West of Tianzhu,M 5. 6 in Danmaand M 4. 7 in Yabulai(Δ≤150 km),as well as M 7. 0 in Gonghe(Δ=270 km) in this paper.Conclusions are follows:( 1)Short-impending ρ_s anomalies up to 10 ̄(-1)─10 ̄(-2) magnitude wererecorded in EW observation direction at the station before the former 4 earthquakes, short-term ρ_s anomalies up to 10 ̄(-2) magnitude which were decreased were recorded before the Gongheand Yabula earthquakes.(2)The short-impending ρ_s anomalies in the direction were probablycaused by the move of ground water along second faults,rifts or fissures in the late period ofseismogenic process, since earth medium within the range of exploration in the direction wasfragmentary. Finaly, author thinks,the reflecting earthquake ability of short-impending ρ_schange in EW direction of the station is higher for moderate and strong earthquakes occurredin certain region around the station.

本文研究了武威地电台周围150km范围内发生的景泰6.2、门源6.4、天祝西4.7、旦马5.6、雅布赖4.7级地震和共和7.0级地震(Δ=270km)该台地电阻率(ρ_s)变化,结果显示:对于前4次地震,该台EW进测值出现10 ̄(-1)─10 ̄(-2)量级的ρ_s短临异常,共和和雅布赖地震前后观测到1O ̄(-1’量级的ρ_s短期下降异常。作者研究认为,ρ_s异常可能是该台EW这探测范围内介质不完整,孕震后期震源力学过程引起地下水沿测区内次级断层、裂隙或裂缝活动造成的。最后本文指出,该台EW道测值对其周围特定位置发生的中强以上地震,在短临阶段映震能力较强。

In this paper,the authors made use of three methods,including slip-average with variableamplitude,slip-residual and massive abrupt rate,to carry out systematically comprehensiveprocessing for those data after groundwater chemistry network established in western Yunnanarea. The correlation analysis between above results and more than 10 M>5. 0 earthquakes inthe neighboring areas shows that this network has very good reflecting earthquake ability,theefficiency of station-point is 0.67 and the efficiency...

In this paper,the authors made use of three methods,including slip-average with variableamplitude,slip-residual and massive abrupt rate,to carry out systematically comprehensiveprocessing for those data after groundwater chemistry network established in western Yunnanarea. The correlation analysis between above results and more than 10 M>5. 0 earthquakes inthe neighboring areas shows that this network has very good reflecting earthquake ability,theefficiency of station-point is 0.67 and the efficiency of station-item is 0.53. The generalresponse earthquake range is less than 100 km. Before earthquakes occurring within thenetwork,all station-items have appeared background anomalies,the earthquake will take placeafter all pionts go into anomaly turning stage. The length of the anomaly duration and themagnitude of the anomaly amplitude are positive correlation with intensity and epicentre dis-tance of the future earthquake. The short information is to be massive abrupt,about 40─50days after massive abrupt rate reached peak and turned,and then the earthquake will occur.Finally,we also discussed the near source field earthquake information observed by thegroundwater chemistry network in western Yunnan area.

在本文中,作者用变幅滑动平均、滑动残差、群体突跳率3种方法,对滇西地区水化观测台网建网以来的资料进行了系统的综合处理,并与邻近地区10多次5级以上地震进行相关分析,结果表明,在台网内发生的地震之前,多数观测点及观测项目都有背景异常显示,异常持续时间长短及幅度大小与地震强度、震中距呈正相关。短期异常表现为群体突跳,当群体突跳率达峰值并发生转折后40─50天地震发生。该台网有较强的映震能力,各观测,点的异常与地震的对应率为67%,观测要素异常与地震的对应率为53%。一般映震范围小于100km。本文最后对滇西区域水化台网观测到的近源场地震信息进行了讨论。

In this paper. we discuss the activity of the Longquanshan fault zone according to faukchorn analysis of determining age sample,test of fault product gas,surveying of crustal deforam-tion and earthquake activity along the fault.Based on the segment characteristics of fault geome-try structure,we made aninquiry into the potential earthquake ability on the fault zone with therelationship between active fault length and earthquake magnitude. the results state clearly thatthe longquanshan fnult zone...

In this paper. we discuss the activity of the Longquanshan fault zone according to faukchorn analysis of determining age sample,test of fault product gas,surveying of crustal deforam-tion and earthquake activity along the fault.Based on the segment characteristics of fault geome-try structure,we made aninquiry into the potential earthquake ability on the fault zone with therelationship between active fault length and earthquake magnitude. the results state clearly thatthe longquanshan fnult zone has been active since Middle-Late Pleislocene Epoch.Since recordinghistorical earthquakes,the bigest earthquake occurred on the fault was the 1967 M5.5 Renshouearthquake. The earthquake activity in recent years is major in medium-small earthquakes. Thefault,therefore, is a medium-strong active fault.The active intensity on the mid-south segmentof the fault is larger than on the north.the active intensity on the west slope has obviously activecharacteristics of separating segment. The bigest magnitude that earthquake will can occur alongthe fault in future ean be M5.5±0.5

本文根据测龄样品的断代分析、地壳形变测量以及沿断裂带的地震活动等对龙泉山断裂带的活动性进行了讨论。并根据断层的几何结构分段特征,运用活断层长度与地震震级的关系,探讨了该断裂带的潜在地震能力。结果表明,龙泉山断裂带属一条中、晚更新世有活动的断裂带。有历史地震史料记载以来,发生最大的一次地震是1967年仁寿大林场5.5级地震,近代地震活动主要以中、小地震活动为主,因此该断裂带属一条中强活动断裂带。从地震活动看,断裂带中南段的活动强度相对北段要大;西坡断裂的活动强度又大于东坡断裂,且西坡断裂具有较明显的分段活动特征。该断裂带上未来可能发生地需的最大震级为5.5±0.5级。

 
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