Reducing interpretation risks in organic-rich low-velocity mudstone using rock physics modeling in Yinggehai Basin, South China Sea
The mudstone in a specific exploration area of the Yinggehai Basin is rich in organic matter and serves as a paradigmatic example of a low-velocity mudstone formation in rock physics. This type of interval exhibits seismic response characteristics similar to those of hydrocarbon reservoirs, which complicates the identification of gas reservoirs and the prediction of gas-bearing zones in this area. In this study, the analysis and modeling of rock physical characteristics within the exploration area are investigated. Based on the actual drilling curve and coring analysis data, a rock physics model of the low-velocity mudstone reservoir is established using self-consistent approximations and the Ciz–Gassmann model, and the influence of organic matter content on the mudstone’s elastic properties is analyzed. Additionally, a robust quantitative inversion procedure is introduced to test the feasibility of inverting for porosity, clay content, and water saturation to mitigate the risk of low-velocity mudstone. The application of actual data, including core samples, logging data, and seismic database, demonstrates the effectiveness of this method and provides technical support for seismic prediction of sand body identification and hydrocarbon detection.
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