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    下扬子无为凹陷北东缘构造演化分析及亚二级构造单元划分

    Structural evolution and sub-secondary tectonic units division of northeast margin in Wuwei Depression, the Lower Yangtze region

    • 摘要: 下扬子地区地质构造较为复杂,中生界和古生界油气勘探尚未取得重大突破。随着勘探程度的不断提高,无为凹陷北东缘显现出巨大的油气资源潜力,亟需划分出更精细的构造单元。文章通过在无为凹陷北东缘系统开展二维地震勘探等地质工作,初步厘定了其深部地震地质结构;以断裂和构造埋深等高线为依据,划分出了6个亚二级构造单元,并结合地质资料,分析了无为凹陷构造演化史。结果表明:无为凹陷北东缘总体经历了平稳震荡期、挤压推覆期和拉张裂陷期,形成现今总体“两洼夹一低凸”的构造格局。研究结果可为无为凹陷后续油气精细勘探提供技术支撑。

       

      Abstract: Due to the complex tectonic of the Lower Yangtze region, oil and gas exploration in the Mesozoic and Paleozoic strata have not been achieved with significant breakthrough. As the advancement of the oil and gas exploration revealed enormous potential for shale gas on the northeast margin of the Wuwei Depression, it’s urgent to delineate sub-level tectonic units. Through 2D seismic and other geological works on the northeast edge of the Wuwei Depression, the deep stratigraphic geological structure was preliminarily determined. Based on faults and structural contour lines, six sub-secondary tectonic units were delineated. Combined with geological data, the tectonic evolutionary stages of the Wuwei Basin are analyzed. Research indicates that the northeast margin of the Wuwei Depression has generally undergone stable oscillation, compressional thrust, and extensional rifting periods, overall presenting a structural pattern of “two depressions sandwich one uplift”. This study will provide technical support for the subsequent fine oil and gas exploration in the Wuwei Depression.

       

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