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天然气地球科学 ›› 2008, Vol. 19 ›› Issue (3): 351–355.doi: 10.11764/j.issn.1672-1926.2008.03.351

• 天然气地质学 • 上一篇    下一篇

苏北盆地海安凹陷下白垩统层序地层和沉积相研究

徐田武,;王英民;魏水建;王文军   

  1. （1.中国石油大学盆地与油藏研究中心,北京 102249 ；2.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 ；3.中国石化石油勘探开发研究院,北京 100083;
    4.江苏油田分公司地质科学研究院,江苏 扬州 225009）
  • 收稿日期:2007-11-05 修回日期:2008-03-13 出版日期:2008-06-10 发布日期:2008-06-10

Characteristics and Evolution of Late Cretaceous Sequence Stratigraphy and Sedimentary Facies in Hai’an Sag

XU Tian-wu1, 2; WANG Ying-min1;WEI Shui-jian3;WANG Wen-jun4   

  1. （1. Basin and Reservoir Research Center, China University of Petroleum, Beijing 102249, China; 2. Ministry of Education Key Laboratory for Hydrocarbon Accumulation Mechanism, China University of Petroleum, Beijing 102249, China; 3. Exploration and Production Research Institute, SINOPEC, Beijing 100083, China; 4. Institute of Geosciences, Jiangsu Oil Company, SINOPEC, Yangzhou 225009, China
  • Received:2007-11-05 Revised:2008-03-13 Online:2008-06-10 Published:2008-06-10

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摘要：

运用地震、测井和分析化验等资料,对苏北盆地海安凹陷下白垩统泰州组进行了层序地层和沉积相研究,将泰州组划分为2个三级层序(泰一段构成层序；1 和泰二段构成层序；2)和5个体系域,其中,层序；1沉积于盆地断陷期, 由于受仪征运动的影响该层序多与下伏浦口组为角度不整合接触,彼此间为典型的层序界面,发育辫状河冲积平原相、辫状河三角洲前缘相、滨—浅湖相和半深湖相沉积;层序；2.形成于盆地拗陷期，主要发育辫状河三角洲前缘相、半深湖—深湖相沉积, 湖泊沉积范围广,湖相暗色泥岩沉积是盆地主要烃源岩。指出海安凹陷生油层主要发育于沉积层序；2中部湖侵体系域的泥灰岩段,该生油层本身又是良好盖层;而储集层则主要发育在沉积层序Ⅰ1和I2顶部的高水位晚期;海安凹陷中心发育的辫状河三角洲前缘及前三角洲砂体是油气的有利勘探区。

关键词: 苏北盆地, 海安凹陷, 下白垩统, 层序地层, 沉积相

Abstract:

This article studies the sequence stratigraphy and sedimentary facies of the Taizhou Formation in the Hai’an sag in the Subei basin using seismic data, well log data, and assaying data. The Taizhou Formation can be divided into 2 third\|order sequences and 5 system fields. Sequence 1 consists of the member 1 of the Taizhou Formation, sequence 2 consists of the member 2 of the Taizhou Formation. The sequence 1 was deposited during the faulting period of the basin, during the period when the plain of braided delta, the front of braided delta and shore\|shallow lake subfacies were developed. Sequence 2 was deposited during the depression period and the shrinking period of the basin, during this period, the front of braided delta and deep facies were developed. The main source rocks were developed in the middle of the TST sequence 2 which is also good capping formation. The sand body reservoirs of lake 2 delta and fan delta were developed during the later period of the HST sequences 1 and 2, and are the potential areas for oil and gas.

Key words: Subei basin, Haian sag, Lower Cretaceous sequence, Sequence stratigraphy, Sedimentary facies.

中图分类号: 

  • TE122.2
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