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在分析了深井资料和地质结构的基础上,恢复了滨里海巨型台向斜东南部的构造发展史,阐明了古构造对盐下层含油气性的影响。
Based on the analysis of deep well data and geological structure, the history of tectonic evolution in the southeast of the giant typhoid in the Caspian Sea is restored, and the influence of paleotectonics on the hydrocarbon-bearing properties of salt subsidence is clarified.