中国石油勘探 ›› 2024, Vol. 29 ›› Issue (4): 111-127.DOI: 10.3969/j.issn.1672-7703.2024.04.009

• 石油地质 • 上一篇    下一篇

渤海青东凹陷北部断垒带沙河街组近源成藏模式

高雁飞,杨海风,赵弟江,康荣,宿雯,王傲林   

  1. 中海石油(中国)有限公司天津分公司
  • 出版日期:2024-07-15 发布日期:2024-07-15
  • 作者简介:高雁飞(1989-),男,湖北荆州人,硕士,2015年毕业于成都理工大学,工程师,现主要从事石油地质综合研究及油气勘探方面的工作。地址 :天津市滨海新区海川路2121 号中海石油(中国)有限公司天津分公司渤海石油研究院,邮政编码:300452。
  • 基金资助:
    国家科技重大专项“渤海海域勘探新领域及关键技术研究”(2016ZX05024—003);中海石油( 中国)有限公司“七年行动计划”重大科技专项课题“渤海油田上产4000 万吨新领域勘探关键技术”(CNOOC-KJ135ZDXM36TJ08TJ)。

Hydrocarbon accumulation pattern near source rock in Shahejie Formation in fault horst zone in the northern Qingdong Sag, Bohai Bay Basin

Gao Yanfei,Yang Haifeng,Zhao Dijiang,Kang Rong,Su Wen,Wang Aolin   

  1. Tianjin Branch of CNOOC (China) Co., Ltd. 
  • Online:2024-07-15 Published:2024-07-15

摘要: 青东凹陷为渤海典型的边缘凹陷,面积小、烃源岩埋深浅,烃源岩的生烃演化机制、有利成藏组合及近源成藏模式不清限制了凹陷油气勘探工作的开展。在区域构造背景分析的基础上,结合地球化学分析、岩石热解、岩石薄片、流体包裹体及埋藏热演化分析,重新认识了青东凹陷的油气成藏条件和勘探潜力。研究表明,沙四上亚段和沙三下亚段是青东凹陷主力烃源岩,沙四段咸化湖盆烃源岩具有早熟生烃演化特征;受郯庐走滑断裂带高热流值影响,烃源岩生烃门限变浅,存在正常热解和浅埋未成熟—低成熟两种生烃机制;区域油源对比表明,北部断垒带原油来源于北部洼陷带的成熟原油和中部洼陷带的低成熟原油;沙四段至沙三段沉积期,青东凹陷内的物源供给能力不断增加,滩坝沉积范围扩张,后转为坝砂沉积,沙三段储层质量向上逐渐变好,薄而广的砂体也可以为油气运移提供良好通道;受古近纪末期的构造反转影响,北部断垒带南部由早期洼陷转变为晚期抬升,局部高点由北部转移向南部;受成藏期流体势驱动,油气从南北两个方向沿断层和砂体呈阶梯式向构造高部位运移成藏。青东凹陷北部断垒带呈现的“双洼供烃—断裂控储—阶梯运聚”的近源汇聚成藏模式,具有典型的渤海边缘凹陷成藏特征,展现了极好的油气勘探潜力。

关键词: 渤海海域, 青东凹陷, 沙河街组, 源储特征, 近源成藏

Abstract: Qingdong Sag is a typical marginal sag in Bohai Bay Basin, with characteristics of small area and shallow burial depth of source rock. The unclear understanding of hydrocarbon generation and evolution mechanisms, favorable hydrocarbon accumulation combinations and hydrocarbon accumulation pattern near source rock restricted the petroleum exploration in the sag. Based on analysis of regional tectonic settings, and combined with study on geochemical experiment, rock pyrolysis, thin section, fluid inclusion and thermal evolution, hydrocarbon accumulation conditions and exploration potential in Qingdong Sag has been re analyzed. The study results show that the upper sub-member of the fourth member and the lower sub-member of the third member of Shahejie Formation served as the main source rocks in Qingdong Sag,and the source rock deposited in saline lake basin in the fourth member of Shahejie Formation showed evolution characteristics of early mature and early hydrocarbon generation; Influenced by high heat flow in Tanlu Strike Slip Fault Zone, the depth threshold of hydrocarbon generation was shallower, and there were two hydrocarbon generation mechanisms of normal pyrolysis and immature-low mature at shallow burial depth;The regional oil and source rock correlation shows that crude oil in the northern fault horst zone was supplied by the mature oil in the northern sub-sag area and low mature oil in the middle sub-sag; During the deposition period from the fourth member to the third member of Shahejie Formation, the sediments supply continuously increased, and the deposition range of beach bar expanded and changed to bar sand deposits in the late stage; The reservoir quality in the third member of Shahejie Formation gradually improved upwards, and the thin and widespread sand bodies provided favorable pathway for hydrocarbon migration; Due to the structural inversion at the end of the Late Paleogene, the southern part of the northern fault horst zone uplifted from an early sub-sag, and local structural high points in the northern part changed to the southern part; Driven by the fluid potential in hydrocarbon accumulation period, oil and gas migrated from north and south directions towards structural high parts along faults and sand bodies in a stepped manner. The hydrocarbon accumulation pattern near source rock shows “hydrocarbon supply by two sub-sags, reservoir controlled by faults, and hydrocarbon migration and accumulation in a stepped manner” in fault horst zone in the northern Qingdong Sag, which is typical in the marginal sag in Bohai Bay Basin, showing excellent exploration potential.

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