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    Computer produces zero-offset vertical seismic profile,
    计算机产生零偏移距垂直地震剖面
    VERTICAL SEISMIC PROFILE MIGRATION KIRCHHOFF INTEGRAL
    垂直地震剖面的克希霍夫积分法偏移
    Application of Pattern Rcognition to Automatically Tracting Seismic Profile Events
    应用模式识别自动追踪地震剖面同相轴
    Vertical Seismic Profile (VSP) Data Error Analysis during Seismic Exploration
    地震勘探中VSP数据的误差分析
    APPLICATION OF LINEARIZED SEISMIC PROFILE IN SEDIMENTARY FACIES RESEARCH
    线性化地震剖面在沉积相研究中的应用
    Identity Method of Gas Hydrate in the Seismic Profile
    地震剖面上的天然气水合物识别方法
    THE FINE VELOCITY STRUCTURE IN THE SHALLOW CRUST ALONG THE HQ?E SEISMIC PROFILE IN SOUTHEASTERN CHINA
    HQ-E爆破地震测深剖面的地壳浅部精细结构及其地质构造研究
    Method for Demarcating through-well Seismic Profile with Diplog and Design of A Microcomputer Software
    地层倾角测井标定过井地震剖面方法研究及微机软件设计
    The strategy of waveform searching in restoration of seismic profile
    地震剖面数据恢复中的波形搜索策略
    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
    THE REALIZATION OF MULTIPAGE PRINTING AND PREVIEW OF SHALLOW SEISMIC PROFILE WITH VC~(++)
    浅层地震剖面多页打印和预览的VC~(++)实现
    THE REALIZATION OF MULTI-PAGE PRINTING AND PREVIEW OF SHALLOW SEISMIC PROFILE WITH VC ~(++)
    浅震剖面分幅多页打印和预览的VC~(++)实现
    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
    2、 The research Sequence Stratigraphy: Combined with the former achievement, the paper distinguish two Ⅰ grade inconformity, two Ⅱ grade inconformity and several Ⅲ grade, Ⅳ grade inconformity from Cambrian-Ordovician of Tazhong area by utilize fully 2-D seismic profile and combine with the well logging and core data.
    2、层序地层划分与研究:在吸收前人研究成果的基础上,充分利用塔中地区二维地震剖面,结合钻(测)井资料,识别出塔中地区寒武—奥陶系的多级不整合面,在此基础上通过连井对比、井震结合等方法对塔中地区寒武—奥陶系进行了层序地层划分,建立了塔中地区寒武—奥陶系综合层序地层格架。
    Texture of the reflection from fault plane shown in seismic profile can be divided into four type: (1) Spoon shaped, (2) Listric shaped, (3)Step shaped and (4)Scarp shaped.
    地震剖面上的断面反射波结构主要有四种类型:(1)勺形、(2)椅形、(3)阶形、(4)坎形。
    Mainly based on seismic profile L_(14) and L_(55), the authors discuss the texture, mode, formation time, thrusting distance and oil and gas prospects of the northern sector of thrusting nappe structure of Longmen Mountains.
    本文以L14、L55地震大剖面为主,论述了龙门山逆冲推覆构造带北段的结构、模式、形成期、推覆距及油气远景。
    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。
    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。
    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。
    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。
 

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