Development of a numerical algorithm for solving the problem of processing and determining the basic velocity model

IF 0.8 Q3 ENGINEERING, PETROLEUM Georesursy Pub Date : 2022-12-20 DOI:10.18599/grs.2022.4.12
A. E. Shumeyko, Vadim A. Tsygankov
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Abstract

This work is devoted to development of an automatic algorithm for determining the velocity model from the data of the field seismic profile. First of all total energy of received signal and the positions of the first arrivals of reflected waves has to be determined. The traces sort by common depth point and the spectra of possible velocities determine at each point of the trace and each assembly of the common deep point. The procedure is fully automated and as a result, instead of about 150 points of manual processing, 4 million points are obtained on the test profile. The values ​​of chosen effective speeds correspond not only to existing criteria for their determination, but also to requirement of smoothness in first derivative. This makes it possible to determine reliable interval velocity profile at each track point and each collection of the common depth point. Speed ​​determination accuracy in the range of 10-50 m/s. After recalculating the time profile into a depth profile, it becomes possible to obtain high-resolution and detailed model of the velocity structure of the geological profile during migration transformations. An iteration process refines the calculations obtained by geologists and geophysicists in order to obtain consistent and consistent results.
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为解决基本速度模型的处理和确定问题,开发了一种数值算法
本文致力于开发一种从现场地震剖面数据中确定速度模型的自动算法。首先,必须确定接收信号的总能量和反射波首次到达的位置。通过共同深度点对轨迹进行排序,并在轨迹的每个点和共同深度点的每个集合处确定可能的速度谱。该过程是完全自动化的,因此,在测试剖面上获得了400万个点,而不是大约150个点的人工处理。所选的有效速度值不仅符合现有的确定标准,而且符合一阶导数的平滑性要求。这使得在每个轨迹点和每个公共深度点的集合上确定可靠的层间速度剖面成为可能。测速精度在10- 50m /s范围内。将时间剖面重新计算为深度剖面后,可以获得地质剖面在运移转换过程中速度结构的高分辨率详细模型。为了得到一致和一致的结果,迭代过程对地质学家和地球物理学家得到的计算进行了改进。
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来源期刊
Georesursy
Georesursy ENGINEERING, PETROLEUM-
CiteScore
1.50
自引率
25.00%
发文量
49
审稿时长
16 weeks
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