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现代地质 ›› 2005, Vol. 19 ›› Issue (Suppl): 228-234.

• 石油地质 • 上一篇    下一篇

山东东营牛庄洼陷南斜坡第三系油气成藏模式

高永进1,2,李雪3,邱桂强1,李素梅4   

  1. 1中国科学院 广州地球化学研究所,广东 广州510640;2胜利油田有限公司 地质科学研究院,山东 东营257015;
    3胜利石油管理局,山东 东营257060;4石油大学 油气成藏机理教育部重点实验室,北京102249
  • 收稿日期:2004-10-10 修回日期:2004-11-30 出版日期:2005-03-20 发布日期:2013-04-08
  • 作者简介:高永进,男, 高级工程师,博士研究生,1968年出生,石油地质学专业,主要从事油田勘探地质的综合研究工作。
  • 基金资助:

    国家“十五”科技攻关项目(2003 BA 613A)。

OIL MIGRATION AND ACCUMULATION MODELS OF THE SOUTH SLOPE OF NIUZHUANG SAG,DONGYING,XHANDONG

GAO Yong-jin1,2,LI Xue3,QIU Gui-qiang2,LI Su-mei4   

  1. 1Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, Guangdong510640, China;
    2Geological Research Institute of Shengli Oilfield Company Limited ,Dongying,Shandong257015 , China;
    3Shengli Petroleum Administuation Bureau,Dongying,Shandong257060,China;
    4Petroleum University,Beijing102249,China
  • Received:2004-10-10 Revised:2004-11-30 Online:2005-03-20 Published:2013-04-08

摘要:

地质与地球化学综合研究表明牛庄洼陷南斜坡第三系不同成因的油气具有不同的成藏模式。下部孔店组成熟度比较高的、混源的油气的形成主要与牛庄洼陷南缘盆倾深切断层的发育有关,致使沙四段烃源岩与孔店组地层直接接触,且沙四段与孔店组成因的油气混合聚集。牛庄洼陷南斜坡第三系油气的分布主要受控于区域构造背景,王家岗-丁家屋子断裂带、八面河断裂—鼻状构造带是上、下层系油气聚集的主要区带。孔店组、沙河街组成因的油气经由断层、砂体运载层与不整合面等沿斜坡上倾方向运移并受优势通道的控制。牛庄洼陷南斜坡第三系不同层系油气的成藏模式及其分布受油源、输导体系、圈闭与储层发育及其分布等多种因素的控制。了解不同层系油气的成藏模式及其主控因素对于油气勘探具有重要的意义。

关键词: 沙河街组, 孔店组, 油气运移, 成藏模式, 牛庄洼陷, 山东

Abstract:

Different oil resources and hydrocarbons accumulation model were identified in the lower Kongdian Formation and upper Shahejie Formation in the south slope of Niuzhuang sag, Bohai Bay.Oil and source rocks correlation showed that oils of Kongdian Formation were derived from deep Ek2 and Es4 members, which have much higher maturity than that of the oils from upper Shahejie Formation. While the oils of the Shahejie Formation and the overlapped formation were sourced from the middle and upper Es4 member within normal oil window. Several faults with hundreds fault throw developed in the southern Niuzhaung sag make it possible that the Es4 source rocks met the Ek1 reservoir resulting in hydrocarbons from the Es4 accumulated in Ek1 strata, which caused the formation of the mixed oils of the Kongdian Formation. It was observed that the oils of the Kongdian, Shahejie formations etc were controlled by main faulted tectonic belts. The oils were distributed in the three tectonic belts including Wangjiagang-Dingjiawozi, Bamianhe and Shicun. The oils migrate through faults, uncomformbilities and sand reservoir etc along upper tilted south slope of the Niuzhuang sag. There are at least two primary hydrocarbons migration pathways having a controlling on oil migration of the area.It was proved that the geological background of Dingjiawozi tectonic belt is suitable to form oil pools of lower Kongdian, while Bamianhe faulted belt is much more suitable to form upper oil pools of Shahejie Formation.The Tertiary hydrocarbon accumulation models of the south slope of the Niuzhuang sag are actually controlled by several factors including oil resource, migration system, traps and the distribution of sand reservoir etc. It is significant for extensive oil exploration to recognize the hydrocarbons accumulation models and their primary controlling factors of different formations of the area.

Key words: Shahejie Formation, Kongdian Formation, oil migration, hydrocarbon accumulation model, Niuzhuang sag, Shandong

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