礁滩相碳酸盐岩地层古地貌恢复方法、装置、设备和介质

By determining the target layer, top surface, and bottom surface of the reef-shoal facies carbonate rock strata, establishing a seismic facies model, identifying bioherms, fitting a depth trend surface, correcting the top and bottom surfaces, determining the compaction coefficient, and generating a paleogeomorphological reconstruction map, the problem of low accuracy in paleogeomorphological reconstruction of reef-shoal facies carbonate rock strata was solved, and quantitative paleogeomorphological reconstruction and reservoir distribution prediction were achieved.

CN116973973BActive Publication Date: 2026-07-17CHINA PETROLEUM & CHEMICAL CORP +1

Patent Information

Authority / Receiving Office
CN · China
Patent Type
Patents(China)
Current Assignee / Owner
CHINA PETROLEUM & CHEMICAL CORP
Filing Date
2022-04-21
Publication Date
2026-07-17

AI Technical Summary

Technical Problem

Existing technologies have low accuracy in paleogeographic reconstruction of reef-shoal carbonate rock strata, and direct analysis using conventional methods is prone to yielding erroneous results.

Method used

By acquiring basic data on reef-shoal facies carbonate rock strata, the top and bottom surfaces of the target layer are determined, a seismic facies model is established, the location of bioherms is identified, the current reef facies depth trend surface is fitted, the top and bottom surfaces are corrected, the compaction coefficient is determined, the stratum thickness and depth are obtained, and a paleogeographic reconstruction map is generated.

Benefits of technology

This method enables quantitative paleogeomorphological reconstruction of reef-shoal facies carbonate rock strata, improving the accuracy of the reconstruction and guiding the prediction of the distribution and development patterns of favorable reef-shoal facies reservoirs.

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Abstract

本发明公开了一种礁滩相碳酸盐岩地层古地貌恢复方法、装置、设备和介质。该方法包括:获取礁滩相碳酸盐岩地层的基础资料信息;基于基础资料信息确定目的层、目的层的顶面和目的层的底面;建立礁滩相碳酸盐岩地层的地震相模式;完成目的层的地震相分析、形成平面地震相分布图,结合地震相模式识别出生物礁的位置,得到生物礁三维空间坐标;根据生物礁三维空间坐标,拟合生成当前礁相深度趋势曲面;根据当前礁相深度趋势曲面校正目的层的顶面和底面;确定压实系数,根据压实系数、校正后的顶面和校正后的底面确定地层厚度和深度;基于地层厚度和深度获得古地貌恢复图。采用本发明,可以准确对礁滩相碳酸盐岩地层进行古地貌恢复。
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