Abstract:Due to multi-stage superposition, small thickness, and complex and varied seismic reflection structures of bioclastic beaches in Maokou Formation of Langzhong area, northern Sichuan Basin, conventional seismic interpretation and prediction methods are not suitable for the identification of bioclastic beaches and the fine characterization of their internal structures. Therefore, with the facies-sequence combination of a single well as the basis, drilling and seismic data are combined to finely calibrate and divide the development stages of bioclastic beaches and determine the seismic reflection characteristics of bioclastic beaches at different stages. The main factors affecting the internal reflection characteristics of bioclastic beaches are analyzed by forward modeling. The global automatic scanning interpretation technique based on sequence stratigraphy is used to accurately depict the internal reflection structure of bioclastic beaches. The seismic attributes that can characterize the distribution characteristics of the bioclastic beaches are selected and combined with the seismic facies to determine the development zone of bioclastic beaches. The sedimentary evolution of clastic beaches at different stages is analyzed in combination with isochronous stratigraphic slicing properties, and the spatial distribution of multi-stage bioclastic beaches is intuitively displayed. The results show that three stages of bioclastic beaches are mainly deve-loped, manifested with "superposed, oblique, cluttered, and weak-amplitude" reflection characteristics. Horizontally, they are distributed in the NW-SE direction;vertically, they are deposited by coating and aggradation from the northeast to the southwest direction in the study area. Dolomite reservoirs are mainly developed in the stage-Ⅲ bioclastic beach. The above results are consistent with the actual drilling results and can provide a basis for future oil and gas exploration.
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