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seismic examples
相关语句
  震例
     COMPREHENSIVE STUDY ON DYNAMIC PATTERNS OF STRAIN STRENGTH RATIO OF FAULT DEFORMATION AND SEISMIC EXAMPLES
     断层形变的应变强度比动态图像与震例综合研究
短句来源
     Accuracy of the dataof this method for land is up to 96% by self-examining,accuracy by seismic examples exami-nation is high too.
     此方法的资料自检准确率陆地达96%,震例检验的准确率也高。
短句来源
     Finally, the relations between field and source in seismic examples is explained by the result about computer model and experimental studies.
     结合计算机模型和实验研究的结果对震例中的场源关系作了解释。
短句来源
     The paper,by confirming normal annual dynamic change of water electrical conductivity in Wayazhi spring and using typical seismic examples analyzed the relationship between annual dynamic change of water electrical conductivity in Wayazhi spring and earthquakes,discussed the reason of causing abnormal changes of water electrical conductivity,and concluded the seismic precursory abnormal is the main reason of changes of water electrical conductivity in Wayazhi spring.
     本文通过确立乌鸦嘴泉水电导率正常年动态变化 ,利用典型震例 ,分析乌鸦嘴泉水电导率年变动态与地震关系 ,讨论了引起水电导率年动态变化畸变的原因 ,并认为地震前兆异常是造成乌鸦嘴泉水电导率变化异常的主要原因
短句来源
     By study of 66 seismic examples in north\|south seismic zone in China,we have known that the main effective factors on the distance between macroseismic epicentre and the epicentre are fault size,fault distribution,fault jointure type and magnitude.
     详细分析南北地震带 66个震例及其与断层空间分布特征的关系 ,以及震源机制解结果后发现 ,影响宏观震中偏离的因素除仪器定位本身的误差外 ,主要还有断层展布方向、活动规模、断层相互交接特征及震级大小等。
短句来源
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  “seismic examples”译为未确定词的双语例句
     SEVERAL SEISMIC EXAMPLES OF TIME CHANGES IN PARAMETERS OF SHORT--PERIOD GEOMAGNETIC VARIATIONS
     短周期地磁变化参量时间变化的几个震例
短句来源
     DETERMINATION OF HYPOCENTER PARAMETERS FOR MODIFIED MODEL AND ANALYSIS OF SEISMIC EXAMPLES
     修正后之孕震模式的震源参数确定及震例分析
短句来源
     Having collected and arranged seismic examples of ground tilt,characteristics of ground tilt anomaly before earthquakes in Jilin area have been summarized in this paper.
     本文清理了吉林省震前地倾斜异常实例,总结了吉林省地倾斜震前异常特征。
短句来源
  相似匹配句对
     Examples of joint inversion of gravimetric and seismic data
     重力、地震资料联合反演实例
短句来源
     Examples are given.
     文中给出了实例.
短句来源
     Combining examples
     本章结合具体实例,
短句来源
     DETERMINATION OF HYPOCENTER PARAMETERS FOR MODIFIED MODEL AND ANALYSIS OF SEISMIC EXAMPLES
     修正后之孕震模式的震源参数确定及震例分析
短句来源
     On seismic resolution
     地震分辨率
短句来源
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In this paper the function of four-phase method to amplify the anomaly of seismic velocities ratio is discussed in greater detail than usual method. It reveals that this method is worth researchinq further and being proved by more seismic examples.

本文对四震相波速比方法较之常规波速比方法具有「放大」波速异常的作用,进行了较详细的讨论,认为四震相波速比是一种值得进一步研究和有待予以更多震例予以验证的方法。

Weak reflection is a reflection phenomenon we can often see in seismic section. The weak reflection is usually considered to come from single-lithologic formation in predicting lithology. The seismic example in Liaodong bay has shown that weak reflection can mirror single-lithologic formation, or multi-lithologic formations: the formation that is composed of thin interbeds,and the formation consisting of thick sandstone and mudstone layers which have very low reflection coefficients. With the use...

Weak reflection is a reflection phenomenon we can often see in seismic section. The weak reflection is usually considered to come from single-lithologic formation in predicting lithology. The seismic example in Liaodong bay has shown that weak reflection can mirror single-lithologic formation, or multi-lithologic formations: the formation that is composed of thin interbeds,and the formation consisting of thick sandstone and mudstone layers which have very low reflection coefficients. With the use of geological model, the author expounds how the weak reflections occur and how they can be distinguished. It is emphasized that the lithology of weak reflection configuration in continental sedimentary basin is determined not only by consulting some interpretation patterns but also by performing com- prehensive analysis of various seismic informations,sedimentary feature and structural feature in the area.

弱反射是地震剖面上常见的一种反射特征,在岩性预测中,一般都解释成单一岩性。根据辽东湾的勘探实例证明,弱反射不只是反映单一名性,也可以在非单一岩性地层中出现,即在薄互层和反射系数很小的厚层砂泥岩地层中产生。笔者利用地质模型论证了它们的形成条件和判别方法,并指出在陆相沉积盆地地层中利用弱反射结构判别岩性,不能简单地运用一两种模式,必须结合本地区的沉积、构造特点,采用多种地震信息进行综合分析。

It is effective to decide whether principal earthquake appears after figure by exponent A(b).The exponent A(b)can distinguish principal earthquake M_L≥5.0 from principalearthquake M_L≤4.7(or no principal earthquake),the principal earthquake size can be alsodetermined with seismic activity region and earthquake intensity data.Accuracy of the dataof this method for land is up to 96% by self-examining,accuracy by seismic examples exami-nation is high too.This method play an important part in seismologic prediction...

It is effective to decide whether principal earthquake appears after figure by exponent A(b).The exponent A(b)can distinguish principal earthquake M_L≥5.0 from principalearthquake M_L≤4.7(or no principal earthquake),the principal earthquake size can be alsodetermined with seismic activity region and earthquake intensity data.Accuracy of the dataof this method for land is up to 96% by self-examining,accuracy by seismic examples exami-nation is high too.This method play an important part in seismologic prediction with fig-ures.

用 A(b)指数判断图象以后有无主震,其效果颇好。A(b)指数能将有主震 M_L≥5.0与有主震 M_L≤4.7(或无主震)区别开来。再加地震活动的范围、强度资料的配合,能判断主震的大小。此方法的资料自检准确率陆地达96%,震例检验的准确率也高。这样的判断,对用图象作地震预报有重要的作用。

 
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