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重力—地震联合剥层预测石柱东部裂陷槽分布

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石柱东部存在震旦—寒武系裂陷槽已经得到地震资料证实,但由于资料的局限性不能准确刻画裂陷槽展布特征.通过大量实测岩石样品和钻井资料分析研究,认识到石柱地区盐酸岩地层密度高,碎屑岩地层密度较低,且不同地层间存在一定的密度差,是重力资料研究深部结构良好的物性基础.因此在石柱地区开展了重力勘探工作,通过针对裂陷槽的重力—地震联合剥层反演技术,确定了石柱东部震旦—寒武系裂陷槽及深部断裂的分布特征.
Prediction of the distribution in eastern Shizhu aulacogen using gravity-seismic formation separation
The existence of Sinian-Cambrian rift troughs in the east of Shizhu has been confirmed by seismic data,but the distribution characteristics of these troughs cannot be accurately described due to the limitations of the data.Through the analysis and study of a large number of measured rock samples and drilling data,it is realized that the density of hydrochloric rock formation is high and the density of clastic rock formation is low in Shizhu area,and there is a certain density difference between different formations,it is a good physical property founda-tion for studying deep structure by gravity data.Therefore,gravity exploration has been carried out in Shizhu area,and the distribution characteristics of Sinian-Cambrian rift troughs and deep faults in the east of Shizhu area have been determined by gravity-seismic combined delamination inversion technique.

Sinian-Cambrian riftgravity-seismic combined delamination inversiondensity differencedeep structure distribution characteristics

吴鹏、王占斌、王财富、赵文举、刘子豪

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中国石油集团东方地球物理勘探有限责任公司综合物化探经理部,河北涿州 072750

震旦—寒武系裂陷槽 重力—地震联合剥层反演 密度差 深部结构分布特征

2024

物探装备
中国石油集团东方地球物理勘探公司

物探装备

影响因子:0.141
ISSN:1671-0657
年,卷(期):2024.34(3)
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