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OALib Journal期刊
ISSN: 2333-9721
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苏北盆地高邮凹陷基底断裂构造特征及成因演化
Keywords: 高邮凹陷,基底断裂,真武断裂,构造特征,成因演化
Abstract:
？基底断裂是深化盆地构造和油气勘探研究的重要领域。以苏北盆地高邮凹陷为研究对象，综合利用钻井、地震、地质、重磁等多元化资料，对基底断裂进行精细构造解释，明确其几何学、运动学特征及成因演化模式。结果表明，高邮凹陷存在一条主干基底断裂(即真武断裂)，平面上呈弯曲线性发育，西段走向nee向、倾向nnw向，东段走向ne向、倾向nw向，剖面上呈铲式发育，后期继承性演化为浅层的真①断层和吴①断层，并发育挤压、反转、伸展、走滑等4类典型构造样式。挤压期和反转期，真武断裂西部活动性强于真武断裂东部活动性；伸展期，真①断层活动性强于吴①断层。在区域动力学分析基础上，分5个阶段解释了高邮凹陷基底断裂的成因和演化。
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