What is it about?
A new combination method flow of seismic wave-field anomaly recognition is proposed. In this process, a robust formation dip scanning is carried out. And, the dip data is applied to the transverse smoothing filter to obtain the formation background data. Then, the seismic wave-field anomaly data is the residual between background data and original seismic data.
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Why is it important?
Distinguish the seismic characteristics caused by deep buried strike-slip fractured zone with high efficiency and high quality, and guide the location of fractured zone.
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This page is a summary of: Seismic Wave Field Anomaly Identification of Ultra-Deep Heterogeneous Fractured-Vuggy Reservoirs: A Case Study in Tarim Basin, China, Applied Sciences, December 2021, MDPI AG,
DOI: 10.3390/app112411802.
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