石油学报 ›› 2023, Vol. 44 ›› Issue (3): 405-419,509.DOI: 10.7623/syxb202303001

• 地质勘探 •    下一篇

中国近海富油凹陷湖相优质烃源岩发育机制

米立军, 张功成, 刘志峰, 陈莹, 白志钊   

  1. 中海油研究总院有限责任公司 海洋油气勘探国家工程研究中心 北京 100028
  • 收稿日期:2022-07-06 修回日期:2023-02-07 出版日期:2023-03-25 发布日期:2023-04-06
  • 通讯作者: 张功成,男,1966年1月生,1994年获西北大学博士学位,现为中海油研究总院有限责任公司教授级高级工程师,主要从事海洋油气勘探地质研究工作。Email:zhanggch@cnooc.com.cn
  • 作者简介:米立军,男,1965年5月生,2007年获中国石油大学(北京)博士学位,现为中海油研究总院有限责任公司教授级高级工程师,主要从事海洋油气勘探管理和综合研究工作。Email:milj@cnooc.com.cn
  • 基金资助:
    国家科技重大专项"中国近海富烃凹陷优选与有利勘探方向预测"(2016ZX05024-002)和中国海洋石油集团有限公司重大课题项目"中国近海盆地潜在富油凹陷资源潜力、成藏机制与突破方向"(2021-KT-YXKY-03)资助。

Discussion on the development mechanism of lacustrine high-quality source rocks in oil-rich sags in offshore China

Mi Lijun, Zhang Gongcheng, Liu Zhifeng, Chen Ying, Bai Zhizhao   

  1. CNOOC Research Institute Co., Ltd.; National Engineering Research Center for Offshore Oil and Gas Exploration, Beijing 100028, China
  • Received:2022-07-06 Revised:2023-02-07 Online:2023-03-25 Published:2023-04-06

摘要: 富油凹陷是大型油气田形成的资源基础,控制或影响着大中型油气田(藏)的形成和富集分布,而优质烃源岩是形成富油凹陷的物质基础,探讨中国近海富油凹陷优质烃源岩发育机制与成因对潜在富油凹陷的遴选意义重大。中国近海已证实的富油凹陷湖相优质烃源岩的发育与分布受控于强断陷、适度遮挡、富营养和热事件4个主要因素。"强断陷"作用可形成深凹陷,为烃源岩的发育提供足够的可容纳空间,同时形成半深湖—深湖还原环境,有利于有机质的富集与保存。烃源岩沉积期,物源搬运路径上的"沉砂池"等对粗碎屑进行"适度遮挡",可控制粗碎屑向凹陷的输入量,使凹陷区特别是深洼区主要发育细粒沉积物形成泥质烃源岩。凹陷及其周缘的深部热液活动、火山灰、流经花岗岩物源区的河流等向凹陷输入丰富的营养物质,导致湖盆水体"富营养",可促进藻类勃发并提供大量沉积有机质,同时形成缺氧环境,有利于优质烃源岩发育。断裂活动和岩浆活动等晚期"热事件"加速了烃源岩热演化,扩大了有效烃源岩的分布范围,有利于烃源岩规模性生油。

关键词: 中国近海, 富油凹陷, 优质烃源岩, 强断陷, 适度遮挡, 富营养, 热事件

Abstract: Oil-rich sag is the resource base for the formation of large oil and gas fields, which controls or affects the formation, enrichment and distribution of large and medium-sized oil and gas fields (reservoirs), and high-quality source rock is the material base for the formation of oil-rich sag. It is of great significance to explore the development mechanism and genesis of high-quality source rocks in oil-rich sags in offshore China for the selection of potential oil-rich sags. The development and distribution of high-quality lacustrine source rocks in proven oil-rich sags in offshore China are controlled by four major factors: strong fault depression, moderate barrier, eutrophication and thermal events. The strong fault depression can form deep sags, providing sufficient accommodation space for the development of source rocks, and forming a semi deep-deep lake reducing environment, which is conducive to the enrichment and preservation of organic matters. During the depositional stage of source rocks, the grit chamber on the provenance migration path moderately blocks the megaclast, which can control the input of megaclast into sags, so that the sag area, especially the deep depression area, mainly develops fine-grained sediments to form argillaceous source rocks. The deep hydrothermal activities, volcanic ash and rivers flowing through the granite provenance area in the sag and its surrounding areas input rich nutrients into the sag, leading to water body eutrophication in the lake basin, which can promote the bloom of algae and provide a large amount of sedimentary organic matters, thus forming an oxygen-deficient environment. This is conducive to the development of high-quality source rocks. Late thermal events such as faulting and magmatism have accelerated the thermal evolution of source rocks, and expanded the distribution range of effective source rocks, which is conducive to the large-scale oil generation of source rocks.

Key words: offshore China, oil-rich sag, high-quality source rocks, strong fault depression, moderate blocking, eutrophication, thermal event

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