声明
1引言
1.1 课题来源、选题依据及意义(Source of topic, research background and significance)
1.2 研究现状和存在问题(The study of status)
1.3 研究内容(Contents)
1.4 研究思路及方法(Research content and method)
1.6 工作量统计(The main work of the thesis)
2 区域地质概况
2.1研究区位置(Location of study area)
2.2地层层序(Stratigraphy sequence)
2.3构造演化(Tectonic evolution)
3湖相细粒沉积岩的沉积学特征
3.1细粒沉积岩综合特征(The character of fine-grained sedimentary rocks)
3.2细粒沉积岩宏观特征(The scheme of lithofacies division)
3.3 细粒沉积岩矿物岩石学特征(Mineralogical and petrological characteristics of fine-grained sedimentary rocks)
3.4细粒沉积岩沉积构造(Sedimentary structure of fine-grained rock)
4岩相类型及其特征
4.1细粒岩岩相划分进展(Lithology facies reviews of fine-grained sedimentary rocks )
4.2细粒岩岩相划分方案(Lithology facies classification)
4.3东营凹陷沙河街组细粒岩相及沉积环境(Lithology facies and depositional environment of Shahejie Formation in Dongying Sag)
4.4沉积演化(Sedimentary environment evolution)
5基于米兰科维奇旋回的细粒沉积岩相成因分析
5.1信号的提取(Signal extraction)
5.2识别结果(Identification results)
5.3 米兰科维奇旋回对细粒沉积岩相的控制(Control on the fine-grained sedimentary rock from milankovic cycles)
5.4 基于米兰科维奇旋回的古气候分析(Paleoclimante analysis based on the Milankovic cycle)
5.5 米兰科维奇旋回控制下的页岩油分布(Shale oil distribution controlled by the Milankovic cycle)
6 结论
参考文献
作者简历
致谢
学位论文数据集
山东科技大学;