摘要
基于有机碳、热解等地化资料,从有机质丰度、类型及成熟度3个方面对乍得Bonger盆地南部凹陷Delo-1井进行烃源岩评价。研究表明:Delo-1井烃源岩暗色泥岩厚度大,有机质丰度高,各层位都达到中等-好烃源岩标准,部分达到最好烃源岩标准;有机质类型主要为I~Ⅱ,型,Kubla组部分为Ⅱ。型;有机质演化处于低熟-成熟演化阶段,其中Baobab组、Ronier组主要处于低熟-成熟演化阶段,Kubla组处于成熟演化阶段,随着深度的增加,成熟度增加。
Based on geochemical data of organic carbon content and pyrolysis etc,the source rocks of Well Delo-1in the southern sag of Bonger Basin were evaluated from abundance and maturity of the organic matter.The results show that the dark mudstones in source rocks of Well Delo-1are thicker,the organic matter abundance is high and each zone reaches the standard of mid-good source rocks,some reach the excellent standard.The organic type is mainly PypeⅠ-Ⅱ1 and some of the Kubla Formation are PypeⅡ2,the organic matter evolution is at low mature-mature stage,Baobab Formation and Ronier Formation are at low mature stage and Kubla Formation is at mature stage.With the increase of depth,the maturity increases.
出处
《石油天然气学报》
CAS
CSCD
2014年第2期19-22,4,共4页
Journal of Oil and Gas Technology