中国石油勘探 ›› 2020, Vol. 25 ›› Issue (6): 79-86.DOI: 10.3969/j.issn.1672-7703.2020.06.008

• 石油地质 • 上一篇    下一篇

南苏丹Melut盆地北部坳陷烃源岩热演化特征及油气地质意义

薛罗,史忠生,马轮,陈彬滔,王磊,马凤良,史江龙   

  1. 中国石油勘探开发研究院西北分院
  • 出版日期:2020-11-12 发布日期:2020-11-12
  • 基金资助:
    国家科技重大专项“大型油气田及煤层气开发”(2008ZX05029);“十三五”中国石油天然气集团有限公司重大科技项 目“海外重点战略大区勘探技术研究与应用”(2019D-4306)。

Thermal evolution characteristics of source rocks in the Northern depression of the Melut Basin, South Sudan, and their petroleum geological significance

Xue Luo, Shi Zhongsheng, Ma Lun, Chen Bintao, Wang Lei, Ma Fengliang, Shi Jianglong   

  1. PetroChina Research Institute of Petroleum Exploration & Development-Northwest
  • Online:2020-11-12 Published:2020-11-12
  • Supported by:
     

摘要: 南苏丹Melut 盆地烃源岩热演化特征研究对盆地油气勘探具有指导意义。通过地质、地球化学资料分 析及含油气系统模拟技术,在恢复北部坳陷热史基础上,利用“Easy% R o”动力学模拟方法模拟计算了Renk 组烃 源岩的成熟史,同时利用“R o—排烃率”模型对Renk 组的生排烃史进行了研究。结果表明,北部坳陷的3 个凹陷 Renk 组烃源岩热演化程度存在一定差异,Jamous 凹陷进入成熟、高成熟、过成熟的时间最早,Ruman 凹陷次之, Moleeta 凹陷最晚。由于热演化史的差异,导致北部坳陷的3 个凹陷在生排烃时间上也具有一定差异性,Jamous 凹 陷在白垩世晚期(88Ma)开始排烃,在古新世进入大规模排烃阶段,而Ruman 凹陷及Moleeta 凹陷进入大规模排 烃阶段的时间在始新世。整体而言,北部坳陷烃源岩生排烃时间与Yabus/Samma 组、Galhak 组与Gayger 组圈闭、 盖层形成时间有良好的匹配关系,影响Yabus/Samma 组成藏的主控因素是油源断裂,而Gayger 组与Galhak 组成 藏的主控因素是储层物性。同时热演化程度高、持续排烃的Renk 组烃源岩为北部坳陷地层—岩性油藏的油气充注提 供了丰富的物质基础。因此,地层—岩性油藏应为北部坳陷重要的勘探接替领域,值得进一步研究探索。

 

关键词: 热演化, 烃源岩, 油气成藏, 盆地模拟, Melut 盆地

Abstract: Study of the thermal evolution characteristics of source rocks in the Melut Basin in South Sudan is of great significance for oil and gas exploration in the basin. Following the restoration of thermal history of the Northern depression, the maturity history of source rocks in the Renk Formation was simulated using the “Easy% Ro” dynamic simulation method combined with the analysis of geological and geochemical data, and petroleum system modeling. Also, the hydrocarbon generation and expulsion history of the source rocks was studied by “Ro - hydrocarbon expulsion rate” model. The results show that there are some differences in the thermal evolution degrees of Renk Formation source rocks between the three sags in the Northern depression. The source rocks in the Jamous sag were the earliest to enter the mature, high mature, and over mature stages, followed by those in the Ruman sag. Source rocks in the Moleeta sag were the most recent. Due to these differences in thermal evolution history, there are also some differences in hydrocarbon generation and expulsion times between the three sags. Source rocks in the Jamous sag began to expel hydrocarbon in the late Cretaceous (88 Ma) and entered the large-scale hydrocarbon expulsion stage in the Paleocene. In the Ruman and Moleeta sags, large-scale hydrocarbon expulsion occurred in the Eocene. Overall, the hydrocarbon generation and expulsion times of source rocks in the Northern depression have a good matching relationship with the formation times of the traps and cap rocks of the Yabus/Samma Formation, Galhak Formation, and Gayger Formation. The main controlling factor for hydrocarbon accumulation in the Yabus/Samma Formation is oil-source connecting faults, while in the Gayger and Galhak Formations it is reservoir physical properties. The source rocks in the Renk Formation, with a high degree of thermal evolution and continuously expelling hydrocarbon, provide a rich material basis for oil and gas charging into stratigraphic-lithologic reservoirs in the Northern depression. Therefore, stratigraphic-lithologic reservoirs should be an important replacement area for future exploration in the Northern depression and deserving of further research and exploration.

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