Hydrocarbon generation and expulsion quantification and contribution of multiple source rocks to hydrocarbon accumulation in Yanchang Formation, Ordos Basin, China

Jingwei Cui , Zhongyi Zhang , Jianliang Liu , Guanglin Liu , Xiu Huang , Yalin Qi , Zhiguo Mao , Yang Li
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引用次数: 5

Abstract

There are several sets of source rocks in the Yanchang Formation of Mesozoic in the Ordos Basin. At present, Chang 7 source rock is considered to be the main source rock of the Yanchang Formation, although there are no evaluation methods for hydrocarbon generation and expulsion of other source rocks, as well as the hydrocarbon accumulation contribution of source rocks. Utilizing basin simulation and based on a large number of basic geological data and exploration results, the geological body model and thermal history model are established to carry out simulation research on hydrocarbon generation, expulsion, and accumulation of multi-source layers in the Yanchang Formation under geological constraints. The results show that the conversion rate of hydrocarbon generation of each source rock in the Yanchang Formation is mainly distributed in the range of 45%–75%, indicating that the formation still has significant hydrocarbon generation potential and has the geological conditions for in-situ exploitation of shale oil. At present, accumulative hydrocarbon generation is 123.3 × 109 t while hydrocarbon expulsion is 90 × 109 t, with heavy hydrocarbons of C14+ dominating. The Early Cretaceous had the highest concentration of hydrocarbon generation and expulsion, accounting for 68%–82% of total hydrocarbon generation and expulsion. The simulation of hydrocarbon accumulation revealed that before the deposition of the Cretaceous, only a limited amount of hydrocarbon charging occurred in each layer of the Yanchang Formation, with the early Cretaceous being the key period of hydrocarbon charging and accumulation. The “near-source accumulation” characterizes the upper and lower hydrocarbon source layers, and the basin simulation results are in good agreement with proven oil reservoirs and predicted oil reservoir distribution ranges. The study proposed for the first time that the “Chang 7 source rock make major contribution to multi-layer reservoir” mode could be modified to “proximal hydrocarbon accumulation from diverse source rock” mode to stimulate shale oil production and potential layer exploration in the Yanchang Formation of Mesozoic in the Ordos Basin.

鄂尔多斯盆地延长组多源岩生排烃量化及对油气成藏的贡献
鄂尔多斯盆地中生代延长组存在多套烃源岩。目前认为长7烃源岩是延长组的主力烃源岩,但对其他烃源岩的生排烃作用及烃源岩的成藏贡献尚无评价方法。利用盆地模拟技术,在大量基础地质资料和勘探成果的基础上,建立地质体模型和热史模型,开展地质约束下延长组多源层生排烃成藏模拟研究。结果表明,延长组各烃源岩生烃转化率主要分布在45% ~ 75%之间,表明该组仍具有显著的生烃潜力,具备原位开采页岩油的地质条件。目前累计生烃123.3 × 109 t,排烃90 × 109 t,以C14+重烃为主。早白垩世生排烃浓度最高,占总生排烃量的68% ~ 82%。油气成藏模拟结果表明,在白垩纪沉积前,延长组各层仅发生少量的油气充注,早白垩世是油气充注成藏的关键时期。上、下烃源层均以“近源聚集”为特征,盆地模拟结果与已探明油藏和预测油藏分布范围吻合较好。研究首次提出了将“长7烃源岩对多层储层贡献较大”模式修改为“多源近端成藏”模式,以促进鄂尔多斯盆地中生界延长组页岩油的开采和潜在层位勘探。
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