ESTIMATION OF COMPENSATION OF INFLUENCE OF LOCAL INHOMOGENEITIES OF THE UPPER PART OF THE SECTION ON A WAVE FIELD IN SEISMIC EXPLORATION

Q3 Earth and Planetary Sciences Geophysical Research Pub Date : 2020-06-01 DOI:10.21455/gr2020.2-2
Удк, Оценка Достоверности, Учета Влияния, Локальных Неоднородностей, Верхней Части, НА Разреза, Волновое Поле, В Сейсморазведке
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Abstract

. A scheme for operational quality control of seismic data processing at the stage of calculating long-period static corrections is proposed. Taking into account long-period velocity inhomogeneities in the upper part of the section by entering static corrections in seismic traces is a generally accepted means of improving the accuracy of structural constructions and is often used in the processing of seismic data. But not always calculated corrections can completely minimize the impact of the upper part of the section. This is primarily due to the fact that underreporting practically does not prevent in-phase summation of useful waves, or, in other words, it does not distort the hyperbolicity of the observed hodograph. The consequences of not taking into account the low-frequency component have a significant impact on the accuracy of determining the kinematic parameters of reflected waves and on further construction of deep surfaces. The proposed method allows you to quickly assess the quality of this compensation. The algorithm for evaluating the quality of accounting for long-period static corrections is based on identifying local deviations in the seismic section of the arrival times of reflected waves and their repeatability at several levels. The information accumulated in this way makes it possible to filter out random and select only regular inhomogeneities. The scheme was tested on several fields in the North of Western Siberia, studied by seismic exploration using the common depth point method and deep drilling. The effectiveness of the algorithm is indirectly confirmed by comparing the detected anomalies with the orohydrography of the research area and on the sedimentation sections of the wave field. The refined morphology of structural surfaces obtained after accounting for long-period distortions should increase the efficiency of seismic exploration.
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地震勘探中剖面上部局部不均匀性对波场影响的补偿估计
。提出了长周期静校正计算阶段地震资料处理的操作质量控制方案。通过在地震迹线中输入静校正来考虑剖面上部的长周期速度不均匀性,是一种普遍接受的提高构造精度的方法,也常用于地震资料的处理。但并不总是计算修正可以完全减少部分的上部的影响。这主要是由于低报实际上并没有阻止有用波的同相求和,或者,换句话说,它没有扭曲观察到的hodograph的双曲线。不考虑低频分量的后果对确定反射波运动参数的准确性和进一步的深表面构造有重大影响。建议的方法允许您快速评估此补偿的质量。评估长周期静校正计算质量的算法是基于识别反射波到达时间的地震剖面的局部偏差及其在几个级别上的可重复性。以这种方式积累的信息使得过滤掉随机而只选择规则的非均匀性成为可能。该方案在西西伯利亚北部的几个油田进行了试验,并采用共深点法和深钻进行了地震勘探研究。将探测到的异常与研究区地形水文和波场沉积剖面进行对比,间接证实了算法的有效性。考虑长周期变形后得到的构造面精细形貌将提高地震勘探的效率。
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来源期刊
Geophysical Research
Geophysical Research Earth and Planetary Sciences-Computers in Earth Sciences
CiteScore
1.00
自引率
0.00%
发文量
19
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