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seismic profiles
相关语句
  地震剖面
    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
    CLASSIFICATION OF SEISMIC PROFILES AND HORIZONTAL CORRELATION OF THREE SHALLOW WAVES
    地震剖面分类与浅层三种波的层位对比
短句来源
    TOMOGRAPHY RESEARCH OF THE ZHEFANG—BINCHUAN AND MENGLIAN—MALONG WIDE—ANGLE SEISMIC PROFILES IN YUNNAN PROVINCE
    云南遮放—宾川和孟连—马龙宽角地震剖面的层析成像研究
短句来源
    Correction of Mis-ties in Seismic Profiles in the Hinterland of the Junggar Basin
    准噶尔盆地腹部地震剖面闭合差的校正
短句来源
    Tectonic interpretation of the seismic profiles in the Lianhuashan area in the southern part of western Sichuan foreland basin
    川西前陆盆地南部莲花山区地震剖面构造解释及构造特征研究
短句来源
更多       
  地震剖面
    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
    CLASSIFICATION OF SEISMIC PROFILES AND HORIZONTAL CORRELATION OF THREE SHALLOW WAVES
    地震剖面分类与浅层三种波的层位对比
短句来源
    TOMOGRAPHY RESEARCH OF THE ZHEFANG—BINCHUAN AND MENGLIAN—MALONG WIDE—ANGLE SEISMIC PROFILES IN YUNNAN PROVINCE
    云南遮放—宾川和孟连—马龙宽角地震剖面的层析成像研究
短句来源
    Correction of Mis-ties in Seismic Profiles in the Hinterland of the Junggar Basin
    准噶尔盆地腹部地震剖面闭合差的校正
短句来源
    Tectonic interpretation of the seismic profiles in the Lianhuashan area in the southern part of western Sichuan foreland basin
    川西前陆盆地南部莲花山区地震剖面构造解释及构造特征研究
短句来源
更多       
  地震剖面
    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
    CLASSIFICATION OF SEISMIC PROFILES AND HORIZONTAL CORRELATION OF THREE SHALLOW WAVES
    地震剖面分类与浅层三种波的层位对比
短句来源
    TOMOGRAPHY RESEARCH OF THE ZHEFANG—BINCHUAN AND MENGLIAN—MALONG WIDE—ANGLE SEISMIC PROFILES IN YUNNAN PROVINCE
    云南遮放—宾川和孟连—马龙宽角地震剖面的层析成像研究
短句来源
    Correction of Mis-ties in Seismic Profiles in the Hinterland of the Junggar Basin
    准噶尔盆地腹部地震剖面闭合差的校正
短句来源
    Tectonic interpretation of the seismic profiles in the Lianhuashan area in the southern part of western Sichuan foreland basin
    川西前陆盆地南部莲花山区地震剖面构造解释及构造特征研究
短句来源
更多       
  “seismic profiles”译为未确定词的双语例句
    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
    Analyses for Bright, Faded and Darken Spots on Seismic Profiles of Carbonate Rocks in Southern Guizhou
    黔南碳酸盐岩地震“亮点”、“平点”与“暗点”分析
短句来源
    SEISMIC STRATIGRAPHIC INTERPRETATION OF HIGH-RESOLUTION SEISMIC PROFILES BETWEEN YANGTZE ESTUARY AND OKINAWA TROUGH
    中更新世以来长江口至冲绳海槽高分辨率地震地层学研究
短句来源
    Transmitted wave field and reflection wave field of simple stratified 3D solid model are sur-veyed with our self-made P-and S- wave transducer on a solid physics analogue test system,through the survey seismic profiles of many mode shapes are obtained.
    在固体物理模拟测试系统上,用自制的纵、横波换能器观测了简单的层状三维固体模型的透射和反射波场,得到了几种振型的地震记录剖面。
短句来源
    In our analysis of waveevents on the seismic profiles,it is found that the wave field resulted from stray vibration of trans-ducer can be recorded while the wave field of different mode shapes resulted from principal vibra-tion is very well recorded in the solid physics analogue study.
    通过分析记录剖面上各种波的同相轴发现,在固体物理模拟实验中,不但能很好地记录到各种报型的主振动波场,还能接收到换能器杂振动引起的波场。
短句来源
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  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.
      
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The elasticity of three silicate garnets with their first pressure derivatives have been experimentally determinated at pressure up to 3.0 GPa using the combination of an ultrasonic interference and piston-cylinder apparatus.This new technique allows us to measure the elasticity at very high precision and the results are:Pyrobe:K0=160.5GPa,μ0=94.5GPa,K'=4.1,μ'=1.37;Grossular:K0=167.9GPa,μ0=86.1GPa,K'=4.9,μ'=1.78;Rhodolite:K0=173.4,μ0=92.5GPa,K'=1.80.Compared with the elastic data from single crystal,the...

The elasticity of three silicate garnets with their first pressure derivatives have been experimentally determinated at pressure up to 3.0 GPa using the combination of an ultrasonic interference and piston-cylinder apparatus.This new technique allows us to measure the elasticity at very high precision and the results are:Pyrobe:K0=160.5GPa,μ0=94.5GPa,K'=4.1,μ'=1.37;Grossular:K0=167.9GPa,μ0=86.1GPa,K'=4.9,μ'=1.78;Rhodolite:K0=173.4,μ0=92.5GPa,K'=1.80.Compared with the elastic data from single crystal,the discrepancy between them is less than 3%(7% for for grossular). It is believed that high quality elasticity data of high pressure phase minerals can be obtained through the polycrystalline if the aggregates if the techniques for the measurement of velocity and pressure,synthesis of high quality sample are avaliable,which is of extremely importance in terms of the interpretation of the seismic profile and the mineral comPosition of the upper-mantle based on these hight pressure phase minerals.

用高精度的液体介质活塞圆筒压力装置和超声干涉技术.在室温和0-3GPa的压力范围内对热压合成的3种石榴子石多晶集合体的波速、弹性模量和它们的压力梯度进行了实验测定.测定的3种石榴子石的体积模量、剪切度量和它们一阶压力梯度分别为:钙-铝榴石:K0=160.5GPa,μ0=94.5GPa,K'=4.1,μ'=1.37;镁-铝榴石:K0=167.9GPa,μ0=86.1GPa,K'=4.9,μ'=1.78;镁铁-钙铝榴石:K0=173.4GPa,μ0=92.SGPa,K'=5.18,μ'=1.80.和单晶体数据相比,其误差小于3%(钙-铝榴石剪切度量误差为7%).用上述方法技术可对更多的幔源矿物在高压下的弹性常数进行直接测定,为上地幔地震波的解释和推论上地幔结构和物质组成提供实验依据

The deep reflection seismic profile plays an important role in deep geological survey.In common circumstances, the omployment of seismograph with wide frequency band reception,proper record fourth and suitable traverse span as well as large dynamic range will help to obtain reflection wave of deep stoeply-dipping interface; with the adoption of large chennel space, fairly lone reception arrangement and rather numerous cover times for data collection,one can not only obtain quite accurate information on...

The deep reflection seismic profile plays an important role in deep geological survey.In common circumstances, the omployment of seismograph with wide frequency band reception,proper record fourth and suitable traverse span as well as large dynamic range will help to obtain reflection wave of deep stoeply-dipping interface; with the adoption of large chennel space, fairly lone reception arrangement and rather numerous cover times for data collection,one can not only obtain quite accurate information on wave velocity and deep reflection wave with high signal to noise ratio, but promote efficiemy and reduce costs as well.

在深部地质调查中,深反射地震剖面发挥了重要作用。一般情况下,在深反射地震调查的数据采集中,采用宽频带接收、适当长的记录长度和测线跨度、大动态范围的地震仪,有利于获取深陡倾斜界面反射波;采用较大的道间距、较长的接收排列和较高的覆盖次数进行数据采集,不但可获取较准确的波速信息、高信噪比的深层反射波,而且也可提高施工效率、降低成本。

The paper gives a result of study integrating the characteristics of seismic reflection waves of 346 seismic profiles in Sichuan, with log data of the gas-water distribution of two carbonate reflectors at the Middle-Lower Triassic(T1-2)erosional surface and the top of the Permian Yangxin Series (P1) in the area. After a study of 172 wells in T1-2 and 109 wells in P1 in the light of the principle of the spacing between the wells and seismic profiles<500 m, it is found that not only the pore-fracture...

The paper gives a result of study integrating the characteristics of seismic reflection waves of 346 seismic profiles in Sichuan, with log data of the gas-water distribution of two carbonate reflectors at the Middle-Lower Triassic(T1-2)erosional surface and the top of the Permian Yangxin Series (P1) in the area. After a study of 172 wells in T1-2 and 109 wells in P1 in the light of the principle of the spacing between the wells and seismic profiles<500 m, it is found that not only the pore-fracture ratio of the sum of wells that show suspicious and non-seismic reflection is 1.3 to 1.6 times that of reliable seismic reflection wells but the high-and intermediate-producing wells among the former are more than those among the latter. Among other things the high-and intermediate-producing wells in the JialingJiang Formation (T1/j) are even 4.7 times higher. It is considered that this is probably the manifestation of the degree of pore-fracture development of the hinterland rocks on the seismic reflection records, thus providing important grounds for predicting the pore-fracture development in the hinterland reservoirs in the area. The suspicious and nonseismic reflection zones in the area are not only widely found in positive structure, but also present often in negative structure. Exploration work shows that gas and water are not distributed according to the model anticlinal traps. There is water in the high part of the anticlinal gas trap and gas outside the trap. This is the manifestation of a fractured gas field with heterogeneous pore-fractures and poor interconnection. Therefore, if gas source is abundant and there exists no deep and large tension fractures, gas may be possibly accumulated in these zones, even in the axial region of a syncline. It follows that the exploration prospect may be expanded greatly and that gas reserves may increase.

根据川西南地区346条地震测线反射波特征,结合实钻资料对该区中下三叠统侵蚀面和二叠系阳新统顶界两个碳酸盐岩反射层的气水分布进行研究后,发现地震可疑+无反射井之和与可靠反射井相比,不仅孔缝发育率前二者之和是后者的1.3—1.6倍,而且高、中产井也较后者多,其中嘉陵江组甚至高达4.7倍。笔者认为这可能是地腹岩层孔缝发育程度在地震反射记录上的反映,从而为预测二叠、三叠系碳酸盐岩储层地腹孔缝发育,拓宽勘探领域,增加储产量提供了重要依据。

 
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