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| 鄂尔多斯盆地东缘上三叠统延长组砂体结构与层序地层学研究 | |
| 引用本文： | 陈飞,罗平,张兴阳,王训练,罗忠,樊太亮,刘柳红,单伟.鄂尔多斯盆地东缘上三叠统延长组砂体结构与层序地层学研究[J].地学前缘,2010,17(1):330. |
| 作者姓名： | 陈飞 罗平 张兴阳 王训练 罗忠 樊太亮 刘柳红 单伟 |
| 作者单位： | 1. 中国地质大学(北京)"海相储层演化与油气富集机理"教育部重点实验室,北京,100083 2. 中国石油勘探开发研究院,北京,100083 3. 中国地质大学(北京)地球科学与资源学院,北京,100083 |
| 基金项目： | 中国石油天然气有限股份公司重大科技攻关项目 |
| 摘 要： | 运用层序地层学原理,对鄂尔多斯盆地东缘上三叠统延长组长7—长4+5曲流河三角洲露头进行深入的研究,划分出低位体系域、湖侵体系域和高位体系域,其内部砂体骨架是由席状化水下分流河道、曲流型分流河道、辫状型分流河道沉积构成。阐述了鄂尔多斯盆地东缘上三叠统延长组层序格架和砂体结构特征,建立了鄂尔多斯盆地层序地层格架内砂体分布模式,构建了层序地层格架内砂体结构与相对湖平面响应模式图。研究表明随湖平面变化层序格架内砂体结构发生规律性变化,低位体系域早期侵蚀,晚期充填呈复合状砂体;湖侵体系域砂体呈孤立状;高位体系域早期砂体发育不全,晚期呈席状砂体。 |
| 关 键 词： | 层序格架 砂体结构 相对湖平面变化 延长组 曲流河三角洲 鄂尔多斯盆地 |
Stratigraphic architecture and sequence stratigraphy of Upper Triassic Yanchang Formation in the eastern margin of Ordos Basin |
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| Chen Fei,Luo Ping,Zhang Xingyang,Wang Xunlian,Luo Zhong,Fan Tailiang,Liu Liuhong,Shan Wei.Stratigraphic architecture and sequence stratigraphy of Upper Triassic Yanchang Formation in the eastern margin of Ordos Basin[J].Earth Science Frontiers,2010,17(1):330. | |
| Authors: | Chen Fei Luo Ping Zhang Xingyang Wang Xunlian Luo Zhong Fan Tailiang Liu Liuhong Shan Wei |
| Abstract: | According to the theory and approach of the sequence stratigraphy,we have investigated the meandering river delta outcrops of the Upper Triassic Yanchang Formation along the eastern margin of Ordos Basin,and identified LST,TST,and HST.Four types of distributary channel depositional systems,including sheetlike subsurface distributary channel,meandering channel and braided channel,which built delta sand body framework,have been identified from the Chang 7 Member to Chang 4+5 Member in Yanchang Formation.Sequence stratigraphic framework and sand body architecture have been illustrated; furthermore,stratigraphic architecture and delta sand-body framework model and sandbody framework related to the relative lacustrine level change have been established.The study demonstrated that the sand-body architecture should have evolved regularly in response to relative lacustrine level change in Ordos Basin; the sand body may have eroded in early LST,and amalgamated channel-filled sand-body was expected in late LST; isolated channel-filled sand-body occurred in TST; during early HST sand body was absent,and sheet-like sand body took place during late HST. |
| Keywords: | sequence stratigraphic framework sandbody architecture relative lacustrine level change Yanchang Formation meandering river delta Ordos Basin |
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