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IDENTIFICATION AND CLASSIFICATION OF SEISMIC REFLECTION VELOCITY PROPERTIES ON SEISMIC REFLECTION SECTIONS

机译:地震反射截面上地震反射速度特性的识别和分类

摘要

1293220 Seismic signal processing PETTY GEOPHYSICAL ENG CO 29 Dec 1970 [5 Jan 1970] 61534/70 Heading H4D A seismic reflection display which includes velocity information is prepared automatically by plotting processed seismic signals as a time or depth section, plotting an overlay representative of interval velocity data and having horizontal and vertical scales in the same ratio as for the seismic section, and superimposing the overlay (e.g. an opaque sheet or a transparency, superimposed directly or by optical projection) on the seismic section. In the Fig. 6 example the seismic section is a depth section and the overlay is in the form of iso-time lines 602 . . . 612. Each such line represents the profile of a hypothetical reflector giving the same two-way seismic travel time at different points along a traverse, taking into account velocity charges such as those due to low velocity zone 601. In the Fig. 5 example the seismic section is a time-section and the overlay is in the form of iso-depth lines such as 102. By comparison with line 102, line 134 is seen to represent a dipping reflector and is not falsely interpreted as showing a structural high below the point 0.5 miles along the traverse. The overlay is preferably coloured differently from the seismic section. Several overlays may be prepared, based on different velocity functions. It is stated that velocity data may be obtained from well logs or from the seismic reflection signals. An overlay based on the velocity down to a reflector causing multiple reflections and on the same velocity for all deeper depths may be used to identify multiple reflections in the seismic section. An automatic data processing system is described in which (a) digitally recorded common depth point (CDP) seismic reflection signals are processed to obtain interval velocity data, (b) normal moveout corrections based on these velocity data are applied to the signals and the corrected CDP signals are stacked, (c) the stacked signals are subjected to further processing including deconvolution and filtering, (d) the processed signals are plotted as a time or depth section, (e) iso-depth or iso-time values are computed from the interval velocity data and (f) these values are plotted as an overlay transparency.
机译:1293220地震信号处理PETTY GEOPHYSICAL ENG CO 1970年12月29日[1970年1月5日]标题H4D通过将处理后的地震信号绘制为时间或深度段,并绘制表示间隔的叠加图,可以自动制备包括速度信息的地震反射显示速度数据,并具有与地震剖面相同比例的水平和垂直刻度,并且在地震剖面上叠加了覆盖图(例如,不透明的薄片或透明体,直接叠加或通过光学投影叠加)。在图6的示例中,地震剖面是深度剖面,并且覆盖层是等时线602的形式。 。 。 612.每条这样的线表示假设的反射器的轮廓,该反射器在沿导线的不同点处给出相同的双向地震传播时间,并考虑了诸如由于低速区601而产生的速度电荷。在图5的示例中,地震剖面是一个时间剖面,覆盖层是等深度线(例如102)的形式。与线102相比,线134被视为代表了一个倾角反射器,并且没有被错误地解释为显示出低于该线的结构高。沿导线指向0.5英里。覆盖层优选地具有与地震部分不同的颜色。基于不同的速度函数,可以准备几个覆盖图。据指出,速度数据可以从测井或地震反射信号获得。基于下降到反射器的速度(导致多次反射)和针对所有更深深度的相同速度的覆盖层可用于识别地震剖面中的多次反射。描述了一种自动数据处理系统,在该系统中,(a)处理数字记录的公共深度点(CDP)地震反射信号以获得区间速度数据,(b)将基于这些速度数据的正常时差校正应用于信号,并进行校正堆叠CDP信号,(c)对堆叠的信号进行进一步的处理,包括解卷积和滤波,(d)将处理后的信号绘制为时间或深度部分,(e)计算等深或等时值间隔速度数据和(f)这些值绘制为覆盖透明度。

著录项

  • 公开/公告号GB1293220A

    专利类型

  • 公开/公告日1972-10-18

    原文格式PDF

  • 申请/专利权人 PETTY GEOPHYSICAL ENGINEERING COMPANY;

    申请/专利号GB19700061534

  • 发明设计人

    申请日1970-12-29

  • 分类号G01V1/00;G01V1/28;

  • 国家 GB

  • 入库时间 2022-08-23 08:04:06

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