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Generation and accumulation of oil and condensates in the Wenchang A Sag, western Pearl River Mouth Basin, South China Sea

机译:南海珠江口盆地西部文昌A凹陷产油和凝析油

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摘要

The Pearl River Mouth (PRM) Basin is one of four Cenozoic basins in the South China Sea, and the Wenchang A Sag is a secondary depression in the western part of the basin. Both the Wenchang and Enping formations contain good source rocks in the western PRM Basin; however, only the latter has been considered a likely source of the discovered oil and gas. New data from fluid inclusions and the analysis of oil-source rock correlations for the WC10-3 oil and gas pools indicate two stages of petroleum charging, the earlier originating from the Wenchang Formation and the later from the Enping Formation. Kinetics of petroleum generation and structural evolution modeling were employed to further investigate the mechanism of formation of the WC10-3 oil and gas pools. It was shown that the crucial condition for the formation of pools is the time of development of the structural trap. The Wenchang Formation source rocks generated oil from 25 to 14 Ma in the possible source area of the WC10-3 oil and gas pools in the Wenchang A Sag, so that only traps formed earlier than this period could capture oil sourced by the Wenchang Formation. The Enping Formation source rock experienced its oil window from 18 Ma to the present with the main stage of oil generation from 15 to 5 Ma. During this period structural traps in the sag continued to form until movements became weak, so that most pools in the Wenchang A Sag originated from the Enping Formation source rock. The likely dissipation of oil and gas from the earlier stage of charging should be taken into account in assessing the oil potential of the Wenchang A Sag.
机译:珠江口盆地是南海四个新生代盆地之一,文昌凹陷是盆地西部的次生凹陷。在PRM盆地西部,文昌组和恩平组均含有良好的烃源岩。但是,只有后者被认为是发现的石油和天然气的可能来源。来自流体包裹体的新数据以及对WC10-3油气藏的油源岩相关性分析表明,石油充注的两个阶段,一个较早的源于文昌组,一个较晚的源于恩平组。运用石油生成动力学和结构演化模型来进一步研究WC10-3油气藏的形成机理。结果表明,池形成的关键条件是构造圈闭的形成时间。文昌组烃源岩在文昌A凹陷WC10-3油气藏可能的烃源区中产生了25〜14 Ma的油,因此只有早于此时期形成的圈闭才能捕获文昌组烃源油。恩平组烃源岩经历了从18 Ma到现在的油窗期,主要的生油阶段从15 Ma到5 Ma。在此期间,凹陷中的构造圈闭持续形成,直到运动减弱为止,因此文昌A凹陷的大部分储层都来自恩平组烃源岩。在评估文昌A凹陷的石油潜力时,应考虑装料早期阶段可能产生的油气耗散。

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