鄂尔多斯盆地延长组地层底面古构造定量化演化及其石油地质意义  

Quantitative Evolution of Paleostructure at the Bottom of the Yanchang Formation in the Ordos Basin and Its Petroleum Geological Significance

作　　者：高胜利 高纪杨 魏雪珂 GAO Sheng-li;GAO Ji-yang;WEI Xue-ke(School of Earth Science and Engineering,Xi'an Shiyou University,Xi'an 710065,China;Key Laboratory of Oil and Gas Reservoir Geology of Shaanxi Province,Xi'an 710065,China)

机构地区：[1]西安石油大学地球科学与工程学院,西安710065 [2]西安石油大学陕西省油气成藏地质学重点实验室,西安710065

出　　处：《科学技术与工程》2024年第5期1782-1788,共7页Science Technology and Engineering

基　　金：陕西省自然科学基础研究计划一般项目(面上)(2019JM-359);西安石油大学研究生创新与实践能力培养计划(YCS2311411,YCS22214204)。

摘　　要：为定量化明确延长组地层在几个关键沉积期的底面凹凸构造面貌特征,基于鄂尔多斯盆地大量钻井等资料并采用盆地模拟技术,划分4个地层单元,即长10~长8、长7、长6~长4+5和长3~长1,定量化考察延长期湖盆在各层地层单元沉积末期的底面古构造特征。结果表明:长8沉积期末,地层底面构造高程整体表现为“东高西低、南高北低”的特征,主湖盆范围的构造等高线在-600 m以下;长7地层沉积期末,整体表现为“南高北低”的古地貌特征,主湖盆范围主要分布在盆地北部、构造高程达-1 150 m以下;长4+5沉积期末,凹陷区分布在盆地西北区域、分布范围和构造高程差变小、约为200 m;长1沉积末期,地层底面构造面貌格局整体表现为“东高西低”的古地貌特征,地层底面凹凸构造高程差为300~400 m。各沉沉积期底面凹凸构造发育,缓坡构造面貌区域是油藏分布的有利区。In order to quantify and define the features of the bottom concave and convex structure of the Yanchang Formation in several key sedimentary periods,four stratigraphic units,namely Chang 10~Chang 8,Chang 7,Chang 6~Chang 4+5 and Chang 3~Chang 1,were divided by basin simulation technology based on a large number of drilling data in Ordos Basin.The paleo structural features of the bottom of the lake basin in the Yanchang period at the end of the sedimentary period of each stratigraphic unit were quantitatively investigated.The results show that at the end of the sedimentary period of Chang 8,the structural elevation of the bottom surface of the formation is“high in the east and low in the west,high in the south and low in the north”,and the structural contour of the main lake basin is below-600 m.At the end of the sedimentary period of Chang 7 Formation,the paleo geomorphology was“high in the south and low in the north”.The main lake basin is mainly distributed in the north of the basin,and the structural elevation is below-1150 m.At the end of the sedimentary period of Chang 4+5,the depression area is distributed in the northwest area of the basin,and the difference between the distribution range and the structural elevation becomes smaller,about 200 m.At the end of Chang 1 Deposition,the overall structural pattern of the bottom of the basin shows a paleogeomorphic feature of“high in the east and low in the west”,and the elevation difference of the concave-convex structure of the bottom of the basin is 300~400 m.The structural features of gentle slope on the bottom of each sedimentation period are favorable areas for reservoir distribution.

关 键 词：地层底面凹凸古构造 主湖盆迁移 油藏分布 鄂尔多斯盆地 

分 类 号：P618.13[天文地球—矿床学] TE121[天文地球—地质学]