尼日利亚东南部阿南布拉盆地生烃模拟:对油气远景的影响。

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摘要

Anambra盆地位于尼日利亚东南部,蕴藏着丰富的油气资源。利用3口探井的数据进行二维(2-D)建模,以评估Anambra盆地的成熟度、生烃时间和分布。目前的研究主要集中在阿南布拉盆地的两个来源,即;Coniacian Agwu和Nkporo烃源岩。模拟结果表明,奥古烃源岩生烃始于晚坎帕尼亚期(77.30Ma)最深沉降区。模型中奥古烃源岩的现今转化率约为60-65%。这一范围表明,奥古烃源岩具有足够的生烃作用。Nkporo烃源岩同样具有生烃能力,但由于其转化率较低(<10%),生烃不足以排烃。Coniacian - Awgu烃源岩的运移烃一定在Coniacian - Agbani和上坎帕尼亚期Owelli砂岩中形成了油气聚集。Amansiodo-1井、Akukwa-2井和Nzam-1井Coniacian Agbani砂岩中发现天然气,表明阿南布拉盆地白垩系地层存在油气圈闭。关键词:二维建模,生排烃,Anambra盆地,转化比,Awgu和Nkporo页岩,
本文章由计算机程序翻译,如有差异,请以英文原文为准。
MODELING HYDROCARBON GENERATION IN ANAMBRA BASIN, SOUTHEASTERN NIGERIA: IMPLICATIONS ON HYDROCARBON PROSPECTIVITY.
The Anambra Basin contains oil and gas producing reservoirs in the southeastern part of Nigeria. Two-dimensional (2-D) modeling, using data from three (3) exploration wells has been carried out to assess the maturity, timing, and distribution of hydrocarbon generation in the Anambra Basin. This current study focuses on two sources in Anambra Basin namely; Coniacian Agwu and Nkporo source rocks. The results of models generated indicate that the onset of hydrocarbon generation from Awgu source rock started in the area of deepest subsidence during the late Campanian (77.30Ma). Awgu source rock in the model has a present-day transformation ratio of about 60-65%. This range indicates that the Awgu source rock has sufficient generation for hydrocarbon expulsion to occur. Nkporo source rock was equally observed to have capacity for hydrocarbon generation, but the generation was insufficient for expulsion because it has lower transformation ratio (<10%). Migrated hydrocarbon from the Coniacian Awgu source rock must have accumulated as oil and gas pools within the Coniacian Agbani and upper Campanian Owelli Sandstone. The discovery of gas in the Coniacian Agbani sandstone of Amansiodo-1, Akukwa-2, and Nzam-1 wells indicates the existence of petroleum traps in Cretaceous beds of the Anambra Basin. Keywords: Two dimensional modelling, Hydrocarbon generation and expulsion, Anambra basin, Transformation ratio, Awgu and Nkporo shales ,
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