中国石油勘探 ›› 2015, Vol. 20 ›› Issue (5): 63-72.

• 海外勘探 • 上一篇    下一篇

巴西东部海域深水盐上碎屑岩油气成藏条件与勘探方向

秦雁群1梁英波1张光亚1巴丹1杨丽丽2吴鹏3   

  1. 1 中国石油勘探开发研究院;2 国土资源部油气资源战略研究中心;3 中联煤层气有限责任公司
  • 出版日期:2015-09-09 发布日期:2015-09-09
  • 基金资助:
    国家科技重大专项全球剩余油气资源研究及油气资产快速评价技术(2011ZX05028);中国石油天然气股份有限公司重大专项全 球油气资源评价与利用技术(2013E-0501)

Hydrocarbon Accumulation Conditions and Further Exploration of Post-salt Clastic Rock in Brazil’s Eastern Deepwater Area

Qin Yanqun1, Liang Yingbo1, Zhang Guangya1, Ba Dan1, Yang Lili2, Wu Peng3   

  1. 1 PetroChina Research Institute of Petroleum Exploration and Development; 2 Strategic Research Center of Oil and Gas Resources, Ministry of Land and Resources; 3 China United Coalbed Methane Co. Ltd
  • Online:2015-09-09 Published:2015-09-09

摘要: 基于国际商业数据库油气田数据和盆地地质与地球物理资料,分析了巴西东部海域深水盐上碎屑岩油气 成藏条件和勘探方向。巴西东部海域盆地群经历了早白垩世凡兰吟期—早阿普特期陆内裂谷、中阿普特期—早阿尔布 期陆间裂谷、中阿尔布期以来的被动大陆边缘3 个演化阶段,横向上可划分为伸展带、底辟带和挤压带。深水盐上碎 屑岩油气来源于巴雷姆阶湖相页岩和赛诺曼阶—三冬阶海相页岩,烃源岩厚度大、品质优,储层物性良好,储盖条件 普遍优越。盐上碎屑岩储层沉积模式显示,其动力学过程为宽缓陆架上驻留的沉积物受触发条件二次搬运、在多点位 置滑塌,在陆架边缘形成平面土豆状定向排列、纵向透镜状分布的浊积体。深水沉积构型主要为无根浊积水道和朵叶 体,储层沉积受盐岩变形限制和改造。深水盐上碎屑岩油气聚集受烃源灶位置、储层沉积相分布和盐岩变形联合控制。 下一步勘探应重点关注陆架边缘内斜坡小盆地,勘探层位向圣埃斯皮里图盆地始新统、渐新统—中新统以及桑托斯盆 地渐新统—中新统横向拓展。

关键词: 巴西;坎普斯盆地;桑托斯盆地;被动大陆边缘;深水;盐岩;盐上

Abstract: Based on the oil and gas field data and basin geological and geophysical data from international commercial databanks, this paper analyzes the hydrocarbon accumulation conditions and exploration areas of deepwater post-salt clastic rock in offshore eastern Brazil. The basins in Brazil’s eastern offshore area experienced three development stages, namely the Early Cretaceous Valanginian – Early Aptian intracontinental rifting stage, the Middle Aptian – Early Albian inter-continental rifting stage, and the passive continental marginal stage after the Middle Albian. Horizontally, the area can be divided into extensional belt, diaper belt and compressional belt. Hydrocarbon of deepwater post-salt clastic rock comes from lacustrine shale from Barremian and marine shale from Cenomanian-Santonian. The source rock is large in thickness and good in quality and physical property, with good reservoir-cap conditions. The sedimentary model of post-salt clastic rock indicates such a dynamic process as the sediments, stayed in the broad continental shelf, is re-transported under triggering conditions and slumped at a number of points. Then turbidite is shaped and laterally and lenticularly distributed in a potato-shaped alignment on the periphery of the continental shelf. The deepwater sedimentary structures are mainly the rootless turbidite channels and lobes while sedimentation of reservoirs is confined and transformed by deformation of salt rock. Hydrocarbon accumulations of deepwater post-salt clastic rock are jointly controlled by source kitchen position, distribution of reservoir sedimentary facies, and deformation of salt rock. The next-stage exploration should be focused on intra-slope ponded-basins on the periphery of continental shelf. The strata of exploration should be expanded horizontally into Eocene and Oligocene – Miocene in Espirito Santo Basin and Oligocene-Miocene in Santos Basin.

Key words: Brazil, Campos Basin, Santos Basin, passive continental margin, deepwater, salt rock, post-salt