CALCULATIONS OF DATUM STATICS IN REFLECTION METHOD WITH CONSIDERATION TO THE POSITION OF THE CHARGE RELATIVE TO THE BASE OF LOWVELOCITY LAYER

Q4 Earth and Planetary Sciences
A. P. Sysoev, A. A. Shamordin
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引用次数: 0

Abstract

While processing ground-based seismic operations by the reflection method using an explosive excitation source, the standard method of compensation technique for the inhomogeneity of the low velocity layer (LVL) is based on the use of blastholes parameters: shot depth, TSP and velocity of underlying stratum, determined by the apparent velocity of refracted wave. The necessary condition for the applicability of this method is the arrangement of the charge below the base of the LVL. Therefore, to substatiate this method, it is necessary to evaluate the position of the charge relative to the roof of the LWL for each source. If the necessary condition for calculating statics computations is not met, it is necessary to solve the problem of estimating the LVL’s thickness and velocity. The presented work contains the problem of analyzing the position of the charge relative to the LVL’s position and estimating the layer parameters which is solving on the basis of joint analysis of the parameters of wells and wave refracted on the LVL base. The solution of the problem is illustrated by the example of real data processing.
考虑电荷相对于低速层基底位置的反射法基准静校正计算
在使用爆炸激发源通过反射法处理地基地震作业时,低速层不均匀性补偿技术的标准方法是基于炮孔参数的使用:炮孔深度、TSP和下伏地层的速度,由折射波的视速度确定。这种方法适用的必要条件是电荷排列在LVL的底部以下。因此,为了取代这种方法,有必要评估每个源的电荷相对于LWL顶部的位置。如果不满足计算静力学的必要条件,就必须解决LVL厚度和速度的估计问题。所提出的工作包括分析装药相对于LVL位置的位置和估计层参数的问题,这是在对井的参数和在LVL基底上折射的波的联合分析的基础上解决的。通过实际数据处理实例说明了问题的解决方法。
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来源期刊
Geology and Mineral Resources of Siberia
Geology and Mineral Resources of Siberia Earth and Planetary Sciences-Geology
CiteScore
0.30
自引率
0.00%
发文量
23
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