| 苏北盆地高邮-海安地区晚白垩世泰州组沉积相及物源分析 |
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| 引用本文： | 徐田武,王英民,曾溅辉,陈莉琼,朱志强,李明刚.苏北盆地高邮-海安地区晚白垩世泰州组沉积相及物源分析[J].地球学报,2007,28(6):627-634. |
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| 作者姓名： | 徐田武 王英民 曾溅辉 陈莉琼 朱志强 李明刚 |
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| 作者单位： | 中国石油大学盆地与油藏研究中心,北京102249;中国石油大学石油天然气成藏机理教育部重点实验室,北京102249;中国石油大学盆地与油藏研究中心,北京102249;中国石油大学石油天然气成藏机理教育部重点实验室,北京102249;中国石油大学盆地与油藏研究中心,北京102249;中国石油大学石油天然气成藏机理教育部重点实验室,北京102249;江苏油田分公司地质科学研究院,江苏扬州225009;中国石油大学盆地与油藏研究中心,北京102249;中国石油大学石油天然气成藏机理教育部重点实验室,北京102249;中国石油大学盆地与油藏研究中心,北京102249;中国石油大学石油天然气成藏机理教育部重点实验室,北京102249 |
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| 摘 要： | 发生在晚白垩世的仪征运动,使泰州组不整合覆盖于赤山组或紫红色浦口组之上.促使了本区南断北超、南陡北缓的箕状断陷的形成与发展,由此导致本区泰一段冲积扇、扇三角洲、辫状河三角洲、半深湖泊沉积相当发育.从盆地边缘到盆地中心,沉积相逐渐由冲积扇沉积渐变为扇三角洲、浅湖、半深湖相沉积.泰二段沉积时期是本区最大湖侵期,半深水湖泊相最为发育.通过对重矿物组合、砂(砾)岩百分含量等值线图及沉积相展布格局等分析认为,本区泰州组沉积时期的物源主要来自南部的苏南隆起、北部的建湖隆起.
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| 关 键 词： | 苏北盆地 高邮凹陷 海安凹陷 泰州组 沉积相 物源 |
Sedimentary Facies and Provenance Analysis of Late Cretaceous Taizhou Formation in Gaoyou-Haian Depression, North Jiangsu (Subei) Basin |
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| XU Tian-wu,WANG Ying-min,ZENG Jian-hui,CHEN Li-qiong,ZHU Zhi-xiang and LI Ming-gang.Sedimentary Facies and Provenance Analysis of Late Cretaceous Taizhou Formation in Gaoyou-Haian Depression, North Jiangsu (Subei) Basin[J].Acta Geoscientia Sinica,2007,28(6):627-634. |
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| Authors: | XU Tian-wu WANG Ying-min ZENG Jian-hui CHEN Li-qiong ZHU Zhi-xiang and LI Ming-gang |
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| Institution: | Key Laboratory for Hydrocarbon Accumulation Mechanism of the Ministry of Education, University of China Petroleum, Beijing 102249; Basin and Research Reservoir Research Center university of Petroleum, Beijing 102249;Key Laboratory for Hydrocarbon Accumulation Mechanism of the Ministry of Education, University of China Petroleum, Beijing 102249; Basin and Research Reservoir Research Center university of Petroleum, Beijing 102249;Key Laboratory for Hydrocarbon Accumulation Mechanism of the Ministry of Education, University of China Petroleum, Beijing 102249; Basin and Research Reservoir Research Center university of Petroleum, Beijing 102249;Geoscience Institute of Jiangsu Oil Company, Sinopec, Yangzhou, Jiangsu 225009;Key Laboratory for Hydrocarbon Accumulation Mechanism of the Ministry of Education, University of China Petroleum, Beijing 102249; Basin and Research Reservoir Research Center university of Petroleum, Beijing 102249;Key Laboratory for Hydrocarbon Accumulation Mechanism of the Ministry of Education, University of China Petroleum, Beijing 102249; Basin and Research Reservoir Research Center university of Petroleum, Beijing 102249 |
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| Abstract: | Yizheng movement occurring in Late Cretaceous led to the unconformable superimposition of Taizhou Formation upon Chishan Formation or Pukou Formation. In this depression, the southern part is characterized by faulting and the northern part by overlapping. As a result, the sediments of fan, fan delta, braided delta and semi-deep lake are well developed in 1st Member of Taizhou Formation. From the edge to the center of the basin, the sedimentary facies change gradually from fan to fan delta or shallow semi-deep lake. During the deposition of 2nd Member of Taizhou Formation, there occurred a big lake transgression in the Gaoyou and Haian Sags, and the semi-deep lacustrine facies was well developed. Based on an analysis of the contour maps of garnet and staurolite, the percentage of sand stones (conglomerates), and the distribution pattern of sedimentary facies, the authors have reached the conclusion that the material sources of the sediments must have been mainly derived from the south of Sunan uplift and the north of Jianhu uplift. |
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| Keywords: | Subei basin Gaoyou sag Haian sag Taizhou formation sedimentary facies Provenance |
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