DYNAMICS OF THE EMISSION RESPONSE OF THE GEOLOGICAL MEDIUM ACCORDING TO MARINE SEISMIC DATA

E. Khogoeva
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Abstract

The present work is devoted to the study of the process of the induced emission of microseisms in an oil reservoir after the passage of elastic waves through it from shotpoint oscillations during seismic exploration. Based on the example of marine seismic data, proven the absence of spectral anomalies of microseisms at the beginning of the traces, before the arrival of waves from the source, and the occurrence of anomalies of medium-frequency microseisms in the 17–23 Hz range at late times of the seismic gathers, after the passage of reflected and multiple waves, were established. The position of the zones of increased emission of microseisms corresponds to oil deposits. In the case of producted oil field, the emission of microseisms is observed, decaying in time, until the end of the recording.
基于海洋地震资料的地质介质发射响应动力学
本文研究了地震勘探过程中弹点振荡的弹性波通过油层后诱发微地震的过程。以海洋地震资料为例,证实了在震源波到达前的迹线起始处微震频谱不存在异常,而在反射波和多次波通过后的地震聚集后期,在17-23 Hz范围内存在中频微震异常。微震发射增加带的位置与油田相对应。对于已开采的油田,观测微震的发射,微震随时间衰减,直到记录结束。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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