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现代地质 ›› 2023, Vol. 37 ›› Issue (05): 1385-1397.DOI: 10.19657/j.geoscience.1000-8527.2023.044

• 油气地质学 • 上一篇    下一篇

加蓬盆地盐下裂谷期碎屑岩储层地球化学特征及物源分析

陈全红1(), 阳怀忠1, 赵红岩1, 张科1, 黄海滨2, 郭家铭1, 刘新颖1, 袁野1   

  1. 1.中国海洋石油国际有限公司,北京 100028
    2.海洋石油工程股份有限公司,天津 300451
  • 收稿日期:2022-06-22 修回日期:2023-04-14 出版日期:2023-10-10 发布日期:2023-11-14
  • 作者简介:陈全红,男,博士,高级工程师,1975年出生,沉积学专业,主要从事沉积-储层学方面的研究。Email:529568@qq.com
  • 基金资助:
    中海油“十四五”重大科技项目“两岸一带重点区油气勘探评价关键技术”(KJGG2022-0902)

Geochemical Characteristics and Provenance Analysis of Clastic Reservoirs in Sub-Salt Rift Period in Gabon Basin

CHEN Quanhong1(), YANG Huaizhong1, ZHAO Hongyan1, ZHANG Ke1, HUANG Haibin2, GUO Jiaming1, LIU Xinying1, YUAN Ye1   

  1. 1. Research Institute of Exploration & Development Technology, CNOOC International Ltd., Beijing 100028, China
    2. Offshore Oil Engineering Co., Ltd., Tianjin 300451, China
  • Received:2022-06-22 Revised:2023-04-14 Online:2023-10-10 Published:2023-11-14

摘要:

加蓬盆地盐下储层物源主要来自上地壳,以长英质岩石为主,主要为元古宙汇聚及俯冲构造背景下的变火山-沉积岩组成的古老变质岩系,同时具有一定量碱性玄武岩和花岗岩的混合。盐下Gamba组及Dentale组地层物源碎屑成分及微量元素与源区构造背景继承性好,不同地层差异不明显。主量元素、微量元素及稀土元素特征值分析表明盐下Gamba组及Dentale组物源主要来自具有沟-弧-盆体系的活动大陆边缘的汇聚及俯冲带,具有低SiO2、Na2O的特征,与刚果克拉通西缘元古宙大陆岛弧背景沉积的基麦赞超群、马永贝超群及西刚果超群等变沉积-火山岩系等有亲缘关系。盆地盐下Gamba组及Dentale组储层具有较高的稀土总量,稀土元素配分模式与刚果克拉通元古宙的西刚果造山带的外部带和中间褶皱带具有亲源性,但与南美圣弗朗西斯科克拉通元古宙—太古宙不同构造活动带差异较大,表明它们不是盆地的主要物源,说明盆地盐下Gamba组及Dentale组物源主要来自刚果克拉通。

关键词: 加蓬盆地, 盐下碎屑岩储层, 主量元素, 微量元素, REE配分模式

Abstract:

Provenance of the subsalt reservoir in the Gabon basin mainly comes from the upper crust, mainly felsic rocks, together with the ancient metavolcanic-sedimentary rocks under Proterozoic convergence and subduction tectonic setting. There is certain amount of mixing of alkaline basalt and granite, with good inheritance of provenance composition and tectonic background of the source region, and no obvious difference. Differences in major and trace element compositions in Gamba and Dentale formations are unobvious. Analyses of major elements, trace elements and rare earth elements show that the provenance mainly comes from the convergence and subduction zones of active continental margin, with trench-Arc basin system. They are featured by low SiO2 and Na2O, similar to the Katanga supergroup and Pore group deposited in Proterozoic back-Arc basin on the western margin of Congo Craton. The Delonggu group is related to each other. The sub-salt reservoirs in the basin have high total REE content. The REE distribution pattern is related to the Proterozoic Lufili orogenic belt on the western margin of Congo Craton, but differs greatly from the Proterozoic Archean tectonic belts of San Francisco Craton in South America. This indicates that they are not the main provenance of the basin, and that the provenance is mainly the Congo Craton.

Key words: Gabon basin, subsalt clastic reservoir, major element, trance element, REE pattern

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