助手标题  
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
   tectonic area 在 地球物理学 分类中 的翻译结果: 查询用时:0.056秒
图标索引 在分类学科中查询
所有学科
地球物理学
地质学
矿业工程
更多类别查询

图标索引 历史查询
 

tectonic area
相关语句
  构造区
    The relation between scalar seismic moment and local magnitude in Tengchong is logM_0=0.98M_L+1048 which is esentially identical to logM_0=0.99M_L+1043 in adjoined Yao'an tectonic area.
    震级与地震矩之间的关系式为logM0=0.98ML+10.48,与姚安构造区得出的结果基本一致;
短句来源
    Study on the spatial evolution of the short-term anomaly of Rn in underground water before strong shocks in the tectonic area of North China and the discrim-inative mark of precursors
    华北构造区强震短期水氡异常空间图像演化及其前兆判别标志的研究
短句来源
    3D seismic exploration of complicated tectonic area in Jiangxi
    江西复杂地质构造区三维地震勘探技术
    It indicates that the SSR method is reliable. (3) Based on the measuring resultsof Lg Q at different stations recorded the same earthquake, it can be seen that thereis obvious difference, which can be regarded as the lateral difference of the toctonicstrucks, on Lg coda Q0 passing through different tectonic area. So if we select someearthquakes with a good azimuth distribuhon and there are a proper stahon distribution,we can image on ofs in the study area using measuring Q.
    (3)对同一地震不同方位各台站的Lg尾波测量结果可以看出,穿过不同构造区的Q_0值存在明显差异,如果这些差异可以看作是构造上横向差异的表现,那么,如果选择方位分布好的一定数量的地震,而记录台站在研究区又具有合适分布,利用这些观测得到的?
短句来源
    The stress drop is in the range of 0.005 MPa to 0.277 MPa. The value at most is only one-fifth of 0.021 MPa~19.4 MPa in Yao'an tectonic area. This might be the answer to the above question.
    地震应力降在(0.005~0.277)×105Pa,仅为姚安构造区地震应力降的1/5。
短句来源
更多       
  构造区
    The relation between scalar seismic moment and local magnitude in Tengchong is logM_0=0.98M_L+1048 which is esentially identical to logM_0=0.99M_L+1043 in adjoined Yao'an tectonic area.
    震级与地震矩之间的关系式为logM0=0.98ML+10.48,与姚安构造区得出的结果基本一致;
短句来源
    Study on the spatial evolution of the short-term anomaly of Rn in underground water before strong shocks in the tectonic area of North China and the discrim-inative mark of precursors
    华北构造区强震短期水氡异常空间图像演化及其前兆判别标志的研究
短句来源
    3D seismic exploration of complicated tectonic area in Jiangxi
    江西复杂地质构造区三维地震勘探技术
    It indicates that the SSR method is reliable. (3) Based on the measuring resultsof Lg Q at different stations recorded the same earthquake, it can be seen that thereis obvious difference, which can be regarded as the lateral difference of the toctonicstrucks, on Lg coda Q0 passing through different tectonic area. So if we select someearthquakes with a good azimuth distribuhon and there are a proper stahon distribution,we can image on ofs in the study area using measuring Q.
    (3)对同一地震不同方位各台站的Lg尾波测量结果可以看出,穿过不同构造区的Q_0值存在明显差异,如果这些差异可以看作是构造上横向差异的表现,那么,如果选择方位分布好的一定数量的地震,而记录台站在研究区又具有合适分布,利用这些观测得到的?
短句来源
    The stress drop is in the range of 0.005 MPa to 0.277 MPa. The value at most is only one-fifth of 0.021 MPa~19.4 MPa in Yao'an tectonic area. This might be the answer to the above question.
    地震应力降在(0.005~0.277)×105Pa,仅为姚安构造区地震应力降的1/5。
短句来源
更多       
  “tectonic area”译为未确定词的双语例句
    Application of Three-dimensional Seismic Exploration Method in Complicated Tectonic Area
    三维地震勘探在构造复杂区的应用
短句来源
    The relevant parameters concerning with magnitude of seismicity for each tectonic area are first calculated.
    研究思路与方法:① 由于构造特征和动力学特征的差异,本文首先将中国大陆分为中国东部地区和中国西部地区。
短句来源
    It is the most active tectonic area of the Eurasia.
    它是地球上陆地隆升最显著的地区,是欧亚大陆现代构造运动最活跃最强烈的地区,也是世界大陆岩石圈构造运动最活跃的地区之一。
短句来源
    The relation between the coda 1/Q c values near the source area of Tianzhu Gulang earthquake and the frequencies have been studied,it shows that the studied area belongs to active tectonic area.
    天祝 -古浪 5 .4级地震震源区附近地区微震尾波 Qc值与频率的关系表明 ,这一地区属于构造活动地区。
短句来源
    Conceiving and occurring of strong earthquake are closely related not only with tectonic area of epicenter but also with whole tectonic zone.
    强震的孕育和发生不仅与震中周围构造有关,而且与孕震区所在的整个构造带有关。
短句来源
更多       
查询“tectonic area”译词为用户自定义的双语例句

    我想查看译文中含有:的双语例句
例句
为了更好的帮助您理解掌握查询词或其译词在地道英语中的实际用法,我们为您准备了出自英文原文的大量英语例句,供您参考。
  tectonic area
If a false alarm is defined as a period of quiescence with a significance level larger than a precursory quiescence in the same tectonic area, then we estimate, based on searches in four areas, that the false alarm rate may be on the order of 50%.
      
Low Pn velocity is observed in southwest Yunnan, Tengchong volcano area, and the Panxi tectonic area.
      
This is why high scattering distribution of heat flow value appears in an active tectonic area, where faults are frequently developed.
      
Now I am testing in the opposite direction, to see if each CMT class produces similarily the same sound-type, independent from the tectonic area.
      


A stacked spectral ratio method is applied to the measurement of Lg coda Q at regional epicentral, distances (△< 500km). In order to test the stability and reliabilityof the method, we select tWo sets of high signal to noise ratio seismic records atdifferent regions. One set is Lg coda bine series from the Beijing telemetry seismicnetwork observed 15 aftershocks of the Datong principal earthquake on Oct 18, 1989(ML = 5.9). Other set is from the portable digital seismic network observed two earthquakes in Pingliang,...

A stacked spectral ratio method is applied to the measurement of Lg coda Q at regional epicentral, distances (△< 500km). In order to test the stability and reliabilityof the method, we select tWo sets of high signal to noise ratio seismic records atdifferent regions. One set is Lg coda bine series from the Beijing telemetry seismicnetwork observed 15 aftershocks of the Datong principal earthquake on Oct 18, 1989(ML = 5.9). Other set is from the portable digital seismic network observed two earthquakes in Pingliang, Gansu province. The source parameters basically are sameaxnong every set of earthquakes, that is to say, their ray paths to the given stationare almost same. So obtained Q can be regarded as an average attenUation effectover the paths, which is not affected by the sources. The measuring Q results showthat: (1) Although there are different instruments used in two seismic netWorks withdifferent observation condihons in every stations, fitting resultS of the Q and ηarehighly linear. It indicates that the SSR method is stable. (2) There are the basicallysame resultS of Lg coda Q at a given station observed different earthquakes of thesame set i,e. Ω0 and their average values are almost within the range of the standarderror. It indicates that the SSR method is reliable. (3) Based on the measuring resultsof Lg Q at different stations recorded the same earthquake, it can be seen that thereis obvious difference, which can be regarded as the lateral difference of the toctonicstrucks, on Lg coda Q0 passing through different tectonic area. So if we select someearthquakes with a good azimuth distribuhon and there are a proper stahon distribution,we can image on ofs in the study area using measuring Q.

将单台记录叠加频谱比法(简称SSR法)应用于震中距小于500km的区域地震Lg尾波为lHz下的值,n是与频率f有关的指数)的提取之中·为了检验方法的稳定性和可靠性,我们选用两组发生在不同地区的地震记录.一组是1989-10-18大同主震(ML=5.9)的15个余震,北京遥测地震台网记录到的信噪比较高的Lg尾波序列。另一组是秦岭造山带数字流动地震观测台网记录到的1995年甘肃平凉两次地震信噪比较高的Lg尾波序列.每一组地震的震源参数基本相同,即它们到某一特定台站的路径几乎相同,得到的 可以认为是不受震源影响的地震一台站路径上的平均衰减效应·两区域 的测量结果表明:(1)尽管两个地震观测台网所用观测仪器不同,每个台站的观测条件不同,所记录的地震也不尽相同,但对Q_0和,的拟合结果线性程度都比较高,说明SSR法是稳定的;(2)同一震群的不同地震到某一特定台站测得的结果基本一致,即Q_0值及其平均值大都在其标准差范围之内,说明SSR法是可靠的。(3)对同一地震不同方位各台站的Lg尾波测量结果可以看出,穿过不同构造区的Q_0值存在明显差异,如果这些差异可以看作是构造上横向差异的表现,那么,如果选择方位分布好的一定数量的...

将单台记录叠加频谱比法(简称SSR法)应用于震中距小于500km的区域地震Lg尾波为lHz下的值,n是与频率f有关的指数)的提取之中·为了检验方法的稳定性和可靠性,我们选用两组发生在不同地区的地震记录.一组是1989-10-18大同主震(ML=5.9)的15个余震,北京遥测地震台网记录到的信噪比较高的Lg尾波序列。另一组是秦岭造山带数字流动地震观测台网记录到的1995年甘肃平凉两次地震信噪比较高的Lg尾波序列.每一组地震的震源参数基本相同,即它们到某一特定台站的路径几乎相同,得到的 可以认为是不受震源影响的地震一台站路径上的平均衰减效应·两区域 的测量结果表明:(1)尽管两个地震观测台网所用观测仪器不同,每个台站的观测条件不同,所记录的地震也不尽相同,但对Q_0和,的拟合结果线性程度都比较高,说明SSR法是稳定的;(2)同一震群的不同地震到某一特定台站测得的结果基本一致,即Q_0值及其平均值大都在其标准差范围之内,说明SSR法是可靠的。(3)对同一地震不同方位各台站的Lg尾波测量结果可以看出,穿过不同构造区的Q_0值存在明显差异,如果这些差异可以看作是构造上横向差异的表现,那么,如果选择方位分布好的一定数量的地震,而记录台站在研究区又具有合适分布,利用这些观测得到的?

Based on a vast amount of first hand materials, the developing features and activities of the 14 NW faults in the area of Beipiao-Yixian are analyzed. The Relation between the two series of faults is also discussed. The result shows that the NW faults and the Chaoyang-Beipiao fault are located in different new tectonic areas, not intersected; also the NW faults have never moved about from late Pleistocene on.

在大量第一手资料的基础上,本文对北票-义县地区分布的14条NW向断裂的发育 特征和活动性进行了研究,并讨论了这一系列NW向断朝阳-北票断裂之间在空间分布 和活动特征上的相关性.结果表明,该地区NW向断裂与朝阳-北票断裂分处于不同的新构 造运动单元,两者在空间上没有交汇;NW向断裂在晚更新世以来没有活动.

The variation characteristics of the coda Q c values of micro earthquakes in the source areas before and after two earthquakes.The two events are Sunan earthquake(M5.7,Nov.22,1988)and Tianzhu Gulang earthquake(M5.4,June 1,1996).The results show that the 1/Q c values tend to identity in the source and its near area before the earthquake M5.7.It is considered that it is a precursor before the earthquake and discussed combining with the source mechanism of this earthquake and the tectonics in the area. The...

The variation characteristics of the coda Q c values of micro earthquakes in the source areas before and after two earthquakes.The two events are Sunan earthquake(M5.7,Nov.22,1988)and Tianzhu Gulang earthquake(M5.4,June 1,1996).The results show that the 1/Q c values tend to identity in the source and its near area before the earthquake M5.7.It is considered that it is a precursor before the earthquake and discussed combining with the source mechanism of this earthquake and the tectonics in the area. The relation between the coda 1/Q c values near the source area of Tianzhu Gulang earthquake and the frequencies have been studied,it shows that the studied area belongs to active tectonic area.

利用张掖台网和天祝 -古浪台网的记录资料研究了 1988年 11月 2 2日肃南 5 .7级地震和 1996年 6月 1日天祝 -古浪 5 .4级地震前后震源区微震尾波 Qc值的变化特征 ,结果表明 :5 .7级地震前震源及邻近地区介质 1/ Qc值趋于一致 ,认为这是该次地震的一种前兆表现 ,结合该次地震的震源机制和构造情况进行了讨论。天祝 -古浪 5 .4级地震震源区附近地区微震尾波 Qc值与频率的关系表明 ,这一地区属于构造活动地区。

 
<< 更多相关文摘    
图标索引 相关查询

 


 
CNKI小工具
在英文学术搜索中查有关tectonic area的内容
在知识搜索中查有关tectonic area的内容
在数字搜索中查有关tectonic area的内容
在概念知识元中查有关tectonic area的内容
在学术趋势中查有关tectonic area的内容
 
 

CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
版权图标  2008 CNKI-中国知网
京ICP证040431号 互联网出版许可证 新出网证(京)字008号
北京市公安局海淀分局 备案号:110 1081725
版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社