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
   seismic profiles 在 地质学 分类中 的翻译结果: 查询用时:0.089秒
图标索引 在分类学科中查询
所有学科
地质学
地球物理学
石油天然气工业
海洋学
矿业工程
新能源
无线电电子学
资源科学
更多类别查询

图标索引 历史查询
 

seismic profiles
相关语句
  地震剖面
    The classification of the lithofacies of the boreholes through the seismic profiles results in the integration of the seismic facies, sedimentary facies and lithofacies analysis and new approach to study sedimentary facies and lithofacies.
    地震相与沉积相的结合,通过地震剖面提供的各种参数解释环境背景和岩相条件,根据地震剖面上所通过的钻井岩相划分,使地震相、沉积相、钻井岩相分析融为一体,并在沉积和岩相研究方法上探索新的途径。
短句来源
    Through the characteristics of geophysical field and the distribution of faults, especially by interpretation of seismic profiles and contrdsting well data, we compared and interpreted seven reflected interfases, Tl, T2, T3, T4, T5, T6 and Tg, of which Tg, T5 and T3 represent three regional unconfondties and are the reflections of three tectonic movements in the Cenozoic sediments of Wanan Basin.
    通过分析区域地球物理场特征及断裂分布,以及地震剖面的解释并结合钻井资料对比分析,在万安盆地新生代沉积中对比解释出T1,T2,T3,T4,T5,T6和Tg等7个地震反射界面。
短句来源
    Seven seismic reflective boundaries (T_1、 T_2、 T_3~1、 T^ T_4、 T_5 and T_g) from up to low are recognized in the seismic profiles of Wan'an basin based on the analysis of seismic re- flective features.
    根据地震反射特征,万安盆地地震剖面由上而下识别出T_1、T_2、T_3、T_3~1、T_4、T_5、T_g共7个地震反射界面。
短句来源
    By using the seismic profiles across the southwest subbasin and the velocity structure and basement of the sediments from the sonobuoy data,together with the drilling data from the shelf that are correlated with those of the strata in the neighboring sedimentary basin, five seismic reflection boundaries have been recognized, named T2,T3,T4,T5,and Tg.
    利用横穿西南海盆的地震剖面,结合声纳浮标资料获得的海盆中沉积物及基底的速度结构,同时结合陆上的钻井分层,并与邻区的沉积盆地地层进行对比,在西南海盆中划分出T2、T3、T4、T5、Tg5个反射界面。
短句来源
    Based on the explanation and structural inversion on the 3D seismic profiles which crossing Chegu201 buried hill, a series of sandbox experiments had been finished.
    在对车古201潜山的三维地震剖面进行解释分析和构造反演的基础上,根据构造模型和相似理论,用砂箱模型模拟了对该区潜山的构造特征及演化过程。
短句来源
更多       
  地震剖面
    The classification of the lithofacies of the boreholes through the seismic profiles results in the integration of the seismic facies, sedimentary facies and lithofacies analysis and new approach to study sedimentary facies and lithofacies.
    地震相与沉积相的结合,通过地震剖面提供的各种参数解释环境背景和岩相条件,根据地震剖面上所通过的钻井岩相划分,使地震相、沉积相、钻井岩相分析融为一体,并在沉积和岩相研究方法上探索新的途径。
短句来源
    Through the characteristics of geophysical field and the distribution of faults, especially by interpretation of seismic profiles and contrdsting well data, we compared and interpreted seven reflected interfases, Tl, T2, T3, T4, T5, T6 and Tg, of which Tg, T5 and T3 represent three regional unconfondties and are the reflections of three tectonic movements in the Cenozoic sediments of Wanan Basin.
    通过分析区域地球物理场特征及断裂分布,以及地震剖面的解释并结合钻井资料对比分析,在万安盆地新生代沉积中对比解释出T1,T2,T3,T4,T5,T6和Tg等7个地震反射界面。
短句来源
    Seven seismic reflective boundaries (T_1、 T_2、 T_3~1、 T^ T_4、 T_5 and T_g) from up to low are recognized in the seismic profiles of Wan'an basin based on the analysis of seismic re- flective features.
    根据地震反射特征,万安盆地地震剖面由上而下识别出T_1、T_2、T_3、T_3~1、T_4、T_5、T_g共7个地震反射界面。
短句来源
    By using the seismic profiles across the southwest subbasin and the velocity structure and basement of the sediments from the sonobuoy data,together with the drilling data from the shelf that are correlated with those of the strata in the neighboring sedimentary basin, five seismic reflection boundaries have been recognized, named T2,T3,T4,T5,and Tg.
    利用横穿西南海盆的地震剖面,结合声纳浮标资料获得的海盆中沉积物及基底的速度结构,同时结合陆上的钻井分层,并与邻区的沉积盆地地层进行对比,在西南海盆中划分出T2、T3、T4、T5、Tg5个反射界面。
短句来源
    Based on the explanation and structural inversion on the 3D seismic profiles which crossing Chegu201 buried hill, a series of sandbox experiments had been finished.
    在对车古201潜山的三维地震剖面进行解释分析和构造反演的基础上,根据构造模型和相似理论,用砂箱模型模拟了对该区潜山的构造特征及演化过程。
短句来源
更多       
  地震剖面
    The classification of the lithofacies of the boreholes through the seismic profiles results in the integration of the seismic facies, sedimentary facies and lithofacies analysis and new approach to study sedimentary facies and lithofacies.
    地震相与沉积相的结合,通过地震剖面提供的各种参数解释环境背景和岩相条件,根据地震剖面上所通过的钻井岩相划分,使地震相、沉积相、钻井岩相分析融为一体,并在沉积和岩相研究方法上探索新的途径。
短句来源
    Through the characteristics of geophysical field and the distribution of faults, especially by interpretation of seismic profiles and contrdsting well data, we compared and interpreted seven reflected interfases, Tl, T2, T3, T4, T5, T6 and Tg, of which Tg, T5 and T3 represent three regional unconfondties and are the reflections of three tectonic movements in the Cenozoic sediments of Wanan Basin.
    通过分析区域地球物理场特征及断裂分布,以及地震剖面的解释并结合钻井资料对比分析,在万安盆地新生代沉积中对比解释出T1,T2,T3,T4,T5,T6和Tg等7个地震反射界面。
短句来源
    Seven seismic reflective boundaries (T_1、 T_2、 T_3~1、 T^ T_4、 T_5 and T_g) from up to low are recognized in the seismic profiles of Wan'an basin based on the analysis of seismic re- flective features.
    根据地震反射特征,万安盆地地震剖面由上而下识别出T_1、T_2、T_3、T_3~1、T_4、T_5、T_g共7个地震反射界面。
短句来源
    By using the seismic profiles across the southwest subbasin and the velocity structure and basement of the sediments from the sonobuoy data,together with the drilling data from the shelf that are correlated with those of the strata in the neighboring sedimentary basin, five seismic reflection boundaries have been recognized, named T2,T3,T4,T5,and Tg.
    利用横穿西南海盆的地震剖面,结合声纳浮标资料获得的海盆中沉积物及基底的速度结构,同时结合陆上的钻井分层,并与邻区的沉积盆地地层进行对比,在西南海盆中划分出T2、T3、T4、T5、Tg5个反射界面。
短句来源
    Based on the explanation and structural inversion on the 3D seismic profiles which crossing Chegu201 buried hill, a series of sandbox experiments had been finished.
    在对车古201潜山的三维地震剖面进行解释分析和构造反演的基础上,根据构造模型和相似理论,用砂箱模型模拟了对该区潜山的构造特征及演化过程。
短句来源
更多       
  “seismic profiles”译为未确定词的双语例句
    Regional Tectonic Characteristics and Significance of North Harbin Area in Songliao Basin: Evidenced from Long Seismic Profiles
    松辽盆地滨北地区区域构造特征及意义——地震长剖面给出的证据
短句来源
    Quaternary Seismic Stratigraphic Interpretation of High-Resolution Seismic Profiles of the South Yellow Sea
    南黄海第四纪高分辨率地震地层学研究
短句来源
    The unconformity T0 3separating the synriftfrom the postrift basin filling represents a breakup unconformity. The unconformities T0 2 and T0 1are regional angular unconformities related to compressive basin inversions. The erosion amounts along these unconformities are about1 0 0 0 m( T03) ,2 5 0 0 m( T02 ) and30 0 0 m( T01) respectively,estimated by modeling and calculation along seismic profiles.
    综合分析表明 ,分隔裂陷和拗陷期充填的 T03 界面代表裂后不整合面 ,T02 和 T01 界面代表了与挤压反转有关的 2个区域性角度不整合 ,其最大剥蚀量分别达 1 0 0 0 m、 2 5 0 0 m和 30 0 0 m。
短句来源
    Maturity distribution and e volution of Cambrian source rocks are delinea ted using software BasinMod-1D on 250wells and 340pseudowells from the 26seismic profiles.
    利用BasinMod-1D软件计算了250口探井,26条地震测线中约340个人工井点有机成熟度随时间的变化,据此编制不同地质时期塔里木盆地台盆区寒武系有机成熟度平面变化图。
短句来源
    ESTIMATION OF RESERVES IN FRACTURED RESERVOIRS——BY APPLICATION OF SEISMIC PROFILES
    裂缝性储集层的储量估算地震剖面图的一种应用
短句来源
更多       
查询“seismic profiles”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。
  seismic profiles
The seismic profiles image several faults, bottom simulating reflectors, and a large rotational slump.
      
Concepts related to Mathematical Information Theory detect some seismic profiles of the refraction experiment which give the most homogeneous coverage of the model in terms of number of trajectories crossing it.
      
From an analysis of many seismic profiles across the stable continental regions of North America and northern Europe, the crustal and upper mantle velocity structure is determined.
      
In 1977, two seismic profiles were carried out in Martinique, one in the area of 'Montagne Pelée' volcano, and the second in the eastern part of the island.
      
In 1976 and 1977, seismic profiles were carried out in Guadeloupe.
      
更多          


Aiming at the actual state of seismic profile being seriously affected by the superficial factors in mountainous regions, the model traces composed by stacking with multiple side-by-side CDP gatherings have been adapted. The model traces having met our needs would tend to be a steady state in the line. In this case the time position simply represents that of zero reference line of static correction. The residual static correction either inside or amidst the gatherings could be completed simultaneously,...

Aiming at the actual state of seismic profile being seriously affected by the superficial factors in mountainous regions, the model traces composed by stacking with multiple side-by-side CDP gatherings have been adapted. The model traces having met our needs would tend to be a steady state in the line. In this case the time position simply represents that of zero reference line of static correction. The residual static correction either inside or amidst the gatherings could be completed simultaneously, if only the traces of the CDP gatherings are pointed to each model trace correspondingly. As a result the signal-to-noiseratio in the sections is then improved, the king amplitude is increased, so as to make shallow, middle and deep reflectors smooth as well as stac continous, the shape of structures become distinct…etc., strictly speaking, it seems to be much superior as compared with the autostatic correction method conducted by imported digital computers 170-4 and 172-4.

山区表层因素严重影响地震剖面的质量,我们采用了多个相邻的CDP道集同相叠加组成模型道,当道数足够多时,模型道在整个测线上趋于稳定,它的时间位置就是静校正零基准线的位置.只要将CDP道集内各道向对应的模型道对齐,就可以同时完成道集内和道集间的剩余静校正.本方法可提高剖面的信噪比,增强叠加能量,使浅中深反射层光滑连续,构造形态清晰……,它比引进的1704和1724机的自动剩余静校正方法更加完善.本方法程序简单,占用内存量小,处理速度快,适用于小型计算机.方法的适应性广泛,无论是弯、直测线;单、多次覆盖剖面都可应用.本方法也可作为修饰性程序应用于地震勘探的数字处理中.

Seismic modelling is an important theoretical problem in seismic prospecting. This paper presents a modelling system in which the ray tracing procedures are used to cal-culate the two-dimensional synthetic seismogram, with finite elements representing com-plicated subsurface structures, thus producing their theoretical section. The system can be applied to the modelling of lithology or geological structures, which would offer use-ful information for the interpretation. A general program for computing...

Seismic modelling is an important theoretical problem in seismic prospecting. This paper presents a modelling system in which the ray tracing procedures are used to cal-culate the two-dimensional synthetic seismogram, with finite elements representing com-plicated subsurface structures, thus producing their theoretical section. The system can be applied to the modelling of lithology or geological structures, which would offer use-ful information for the interpretation. A general program for computing arbitrary complicated structures has been prepared. It proved effective in calculating a series of models for a certain seismic profile. These synthetic sections were displayed on tele-vision. The paper ends with a brief discussion and analysis of the results thus obtained.

复杂地层构造的地震模拟,是地震勘探理论的重要问题。本文提出了一个模拟系统:用有限元素表示复杂地层构造,在此基础上应用射线轨迹法计算二维合成记录,从而得到复杂地层构造的理论剖面。这个系统可以用来模拟构造和岩性,为解释人员提供理论依据。 作者研制了适用于任意复杂地层构造计算的通用程序,并用以计算了某测线的一批模型,所得合成剖面由电视加以显示,最后对结果作了简单的分析讨论。

During the past 4 years (1975-1979) eight seismic profiles have been compiled by using the method of earthquake-generating converted waves in the Beijing-Tianjin-Tangshan region. Some details about the method of interpretating these data and the important results obtained are presented in this paper. This method is very useful in the regional investigations for earth's crust and upper mantle.The comparison of the deep-seated structures and the distribution of earthquakes in the studied region indicates...

During the past 4 years (1975-1979) eight seismic profiles have been compiled by using the method of earthquake-generating converted waves in the Beijing-Tianjin-Tangshan region. Some details about the method of interpretating these data and the important results obtained are presented in this paper. This method is very useful in the regional investigations for earth's crust and upper mantle.The comparison of the deep-seated structures and the distribution of earthquakes in the studied region indicates that all hypocentres of strong earthquakes just filled in some particular position of the granitic layer and that the Tangshan and Mafan strong earthquake regions are similar each other in the deep-seated structure characteristics, such as relative uplift of the granitic layer, intensive depression (concavity) of interfaces in upper mantle, sharp thickening of lithosphere and existence of deep-seated faults in the region under investigation.

1975—1979年间在京津唐地区完成了八条地震转换波测深的剖面工作,本文介绍所取得的主要成果。结果表明转换波法用于地壳、上地幔深部结构的探测是有效的。深部构造剖面与震源分布的对比表明,本区几乎所有强震震源都分布在“花岗岩”层的某些特殊部位上。唐山和马坊大震地区的深部构造具有相似的特征,这就是“花岗岩”层的相对隆起,上地幔界面的强烈凹陷,岩石圈相应地急剧增厚以及存在深大断裂。

 
<< 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seismic profiles的内容
在知识搜索中查有关seismic profiles的内容
在数字搜索中查有关seismic profiles的内容
在概念知识元中查有关seismic profiles的内容
在学术趋势中查有关seismic profiles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