| 渤海海域古近系湖盆边缘构造样式及其对沉积层序的控制作用 |
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| 引用本文： | 徐长贵,于水,林畅松,王昕,王粤川,李慧勇.渤海海域古近系湖盆边缘构造样式及其对沉积层序的控制作用[J].古地理学报,2008,10(6):627-635. |
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| 作者姓名： | 徐长贵 于水 林畅松 王昕 王粤川 李慧勇 |
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| 作者单位： | 1.中海石油（中国）有限公司天津分公司技术部，天津塘沽300452;2.中海石油研究中心，北京100027;3.中国地质大学（北京）能源学院，北京100083 |
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| 基金项目： | 国家科技攻关计划
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| 摘 要： | 陆相断陷湖盆边缘构造带是湖盆的重要组成部分，它们通常紧邻生油中心，是陆相断陷湖盆的油气主要富集带之一。渤海海域古近系湖盆边缘构造样式可划分为伸展型湖盆边缘和走滑型湖盆边缘两大类，伸展型湖盆边缘又可划分为陡坡断裂型湖盆边缘、缓坡断裂型湖盆边缘、简单缓坡带型湖盆边缘和轴向斜坡型湖盆边缘。伸展型湖盆边缘在全区各大凹陷均可见，走滑型湖盆边缘仅发育在盆地的东部地区，主要受郯庐断裂带的控制。不同类型湖盆边缘的构造活动方式和构造演化过程各不相同，因而其所形成的地貌形态有较大的差别，可容空间和沉积基准面的变化各具特色，从而导致不同构造样式的湖盆边缘具有不同的沉积层序构成模式。湖盆边缘构造样式对层序构成的控制作用的分析对储集层预测和岩性圈闭预测具有重要的指导意义。
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| 关 键 词： | 伸展型湖盆边缘 走滑型湖盆边缘 构造样式 层序构成 古近系 渤海 |
Structural styles of the Paleogene lacustrine basin margin and their control on sedimentary sequences in Bohai Sea area |
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| Xu Changgui,Yu Shui,Lin Changsong,Wang Xin,Wang Yuechuan,Li Huiyong.Structural styles of the Paleogene lacustrine basin margin and their control on sedimentary sequences in Bohai Sea area[J].Journal of Palaeogeography,2008,10(6):627-635. |
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| Authors: | Xu Changgui Yu Shui Lin Changsong Wang Xin Wang Yuechuan Li Huiyong |
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| Institution: | 1.Technical Department of China National Offshore Oil Corporation Limited Tianjin， Tanggu300452， Tianjin;2.Research Center of China National Offshore Oil Corporation， Beijing100027;3.School of Energy，China University of Geosciences(Beijing)， Beijing100083 |
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| Abstract: | As an important part of continental rift lacustrine basin,the structural zones of the basin margin which are usually located close to the hydrocarbon-generating center,are important petroliferous belts in the continental rift lacustrine basin.In the Bohai Sea area,the structural styles of the Paleogene lacustrine basin margin can be divided into two types:extensional lacustrine basin margin and strike slipping lacustrine basin margin and the former one is further subdivided into the steep slope faulted lacustrine basin margin,the gentle slope faulted lacustrine basin margin,the simple gentle slope lacustrine basin margin and the axial slope lacustrine basin margin.The extensional lacustrine basin margin is widely distributed in the large sags of the study area,while the strike slipping one is developed in the eastern area of the basin and is mainly controlled by the Tancheng-Lujiang faulted belt.Due to the differences of the structural movements,the structural evolution of different lacustrine basin margins,the palaeogeomorphology,the accommodation variation and the sedimentary base level changes are different.As a result,different lacustrine basin margins with different structural styles have different sedimentary sequence filling models.The analyses of the control of lacustrine basin margin structural styles on sequence filling are very important for reservoir delineation and prediction of lithologic traps. |
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| Keywords: | extensional lacustrine basin margin strike slipping lacustrine basin margin structural style sequence constitution Paleogene Bohai Sea |
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