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1)  precursory difference
前兆差异性
1.
Taking these two earthquakes as the samples, the precursory differences between grouped strong earthquakes and the single strong earthquake are studied.
以 1 995与 2 0 0 0年发生在云南楚雄地区武定、姚安的两次 6 5级强震为例 ,研究了成组强震和单个强震的前兆差异性
2)  Electric precursor anomaly
电性前兆异常
3)  precursory anomaly
前兆异常
1.
Based on the synthetic math expression of earthquake precursory anomaly information variable in this paper,we acquired the S-values according to the information with precursory anomaly provided by 11 seismic stations and non-precursory anomaly by 7 seismic stations before Xiuyan 5.
本文以地震前兆异常信息量综合数学表达式为基础,结合平滑滤波、消周期及趋势项和从属函数等数据处理方法,对1999年11月29日岫岩5。
2.
Based on the mechanism to induce groundwater anomaly,the interferences of precursory anomaly and its recognition are discussed,and the view of "rain and groundwater interference"is questioned.
按照地下水诱发异常的机理,讨论了诱发前兆异常的干扰与识别问题,并对"降水、地下水干扰"观点提出质疑。
4)  Precursory anomalies
前兆异常
1.
Before the two events,a lot of precursory anomalies of subsurface fluid appeared in north Tianshan mountations area,but there is clearly difference in the anomalies before the two events.
7级地震 ,两次地震前 ,北天山地区地下流体都相继出现了不少前兆异常 ,但两次前兆异常也存在着明显差异。
5)  Precursory Abnormity
前兆异常
1.
Discussion on precursory abnormity of water chymistry mechanism in Wutazui spring;
福州乌鸦咀泉水化学前兆异常机理探讨
2.
There appeared orderly precursory abnormity of underground fluid in the northern Tienshan mountain before the earthquake,and most of them is mid-short term abnormity,concentrating on around Urumqi,which is 265 km or so from the epicenter.
7地震,震前北天山地区的地下流体相继出现一些前兆异常,并且以中短期异常为主,异常主要集中在距震中约265 km的乌鲁木齐附近。
6)  Precursor anomaly
前兆异常
1.
The Research of Precursor Anomaly Characteristic of Ground Resistivity Anisotropy and Its Physical Mechanism in Earthquake;
地电阻率各向异性前兆异常特征及其与地震的关系
2.
Based on the method of anomaly recognition and mark system for the precursor subject, the characteristics of precursor anomaly of the ground fluid have been identified and studied during the Heze M59 earthquake in 1983 and the features of stages, layer and synchronism of precursor anomaly of ground fluid were analyzed.
9级地震前地下流体前兆异常特征进行了识别与研究,分析了菏泽5。
3.
Therefore,we consider that using wavelet transform method to extract seismic precursor anomaly is efficient.
因此,运用小波分析方法可以有效地提取地震前兆异常信息。
补充资料:差异性发绀


差异性发绀
different cyanosis

  表现为头颈及上肢无发绀,而躯干及下肢出现发绀,并可伴有杵状趾,是由于一部分静脉血经异常通道流入降主动脉而产生。多见于主动脉弓中断并发动脉导管未闭和室间隔缺损的病例,或复杂的主动脉缩窄及动脉导管未闭并发肺动脉高压出现双向分流或右向左分流的病例。
  
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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