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OALib Journal期刊
ISSN: 2333-9721
费用：99美元
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伊宁凹陷构造沉降史与主控因素分析
Keywords: 伊宁凹陷,古生代,沉降史,剥蚀厚度,陆内裂陷
Abstract:
？利用伊宁凹陷多口钻/测井、模拟井及地震数据估算了侏罗纪末期地层剥蚀量，且在充分考虑多种因素基础上，应用回剥技术模拟分析了该区中二叠世以来构造沉降史。研究表明，伊宁凹陷中二叠世以来主要经历了3次快速沉降、2次缓慢沉降与2次区域性快速抬升剥蚀的过程。其中，中二叠世—早三叠世为最大构造沉降期，沉降中心位于中央凹陷带霍城地区，海西期火山裂谷后热沉降作用是造成此次沉降的直接因素；早侏罗世与新近纪以后沉降次之，构造运动形成的差异性升降规律是这2次快速沉降的主要成因；侏罗纪末期—白垩纪早期为主要剥蚀抬升期，伊宁凹陷西部剥蚀强度远远大于东部地区，具有明显的东西差异性。？
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