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METHOD FOR PERIODICALLY MEASURING TIME THICKNESS OF SEDIMENTARY STRATUM USING RECEIVER FUNCTION

机译:接收函数周期性测量沉积地层时间厚度的方法

摘要

A method for periodically measuring the time thickness of a sedimentary stratum using a receiver function, belonging to the field of solid geophysical research. The method comprises: firstly selecting a vertical component Z, a radial component r and a tangential component t of three component seismic data, received by a seismic station, the magnitude thereof being more than four and the epicentral distance thereof being 30 degrees to 100 degrees, and selecting seismic events satisfying the condition; then respectively calculating normalized autocorrelation functions of the vertical component Z, the radial component r and the tangential component t for each of the seismic events; detecting whether each seismic event i is periodic and determining whether the periodicity of the seismic event i is a periodicity caused by a sedimentary stratum below a receiving station; and obtaining an average time thickness reflecting the thickness of the sedimentary stratum below the seismic station by using a mathematical average algorithm. The method provides a theoretical basis for the research of a sedimentary stratum.
机译:一种使用接收器功能定期测量沉积层时间厚度的方法,属于固体地球物理研究领域。该方法包括:首先选择地震台站接收的三分量地震数据的垂直分量Z,径向分量r和切向分量t,其震级大于4,震中距离为30度至100度。 ,并选择满足条件的地震事件;然后分别计算每个地震事件的垂直分量Z,径向分量r和切向分量t的归一化自相关函数。检测每个地震事件i是否是周期性的,并确定地震事件i的周期性是否是由接收站下方的沉积地层引起的周期性;通过使用数学平均算法,获得反映地震台下沉积层厚度的平均时间厚度。该方法为研究沉积地层提供了理论依据。

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