南海东部大中型富糯米质油气田的发现与启示:以珠江口盆地惠州26子囊古近纪恩平地层为例

IF 7 Q1 ENERGY & FUELS
Changgui XU , Yangdong GAO , Jun LIU , Guangrong PENG , Pei LIU , Wanlin XIONG , Penglin SONG
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引用次数: 0

摘要

以珠江口盆地惠州下陷油气勘探实践为基础,测定了源岩地球化学指标,恢复了储层发育形态,进行了岩石矿物显微特征描述,对比了圈闭实测指标,提取了原油生物标志化合物,查明了凝析气成因,研究了成藏条件。在此基础上,系统分析了惠州26亚格古近系恩平地层油气资源潜力、大型优质砾岩储层发育特征、断层圈闭有效性、油气运移与富集模式、大中型富糯米质油气田成藏条件与勘探目标。研究成果主要体现在四个方面。第一,惠州26亚格古近系文昌地层发育广厚的半深-深湖相亚基性优质源岩,具有典型的 "前期大量生油,后期大量排气 "的烃类运移特征,为恩平地层的烃类聚集提供了充分的物质基础。其次,在陡坡带和下陷内断层过渡带的共同控制下,近源大型谷朊岩储层具有高度异质性,其发育规模受三个因素(有利面带、颗粒组分和微裂缝)的分级控制。断层系统附近的(水下)分布通道,颗粒均等、含泥量低(<5%)、长石成分含量高,有利于甜点储层的发育。第三,稳定的湖漫泥岩覆盖的走向滑动加压陷阱是油气保存的必要条件,与主应力斜交的NE向和近EW向断层对陷阱的控制作用最好。第四,优质源岩、断层运移/封堵和糯米质储层的时空配置控制着油气富集程度。从上到下,可划分为三个油气富集单元,即低充填区、过渡区和高充填区。近压源连接断裂带的主要通道区域有利于大规模油气富集。该研究成果为珠江口盆地恩平地层大型富含糯米质油藏的勘探提出了新的方向,是油气勘探的重大突破。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Discovery and inspiration of large- and medium-sized glutenite-rich oil and gas fields in the eastern South China Sea: An example from Paleogene Enping Formation in Huizhou 26 subsag, Pearl River Mouth Basin

Based on the practice of oil and gas exploration in the Huizhou Sag of the Pearl River Mouth Basin, the geochemical indexes of source rocks were measured, the reservoir development morphology was restored, the rocks and minerals were characterized microscopically, the measured trap sealing indexes were compared, the biomarker compounds of crude oil were extracted, the genesis of condensate gas was identified, and the reservoir-forming conditions were examined. On this basis, the Paleogene Enping Formation in the Huizhou 26 subsag was systematically analyzed for the potential of oil and gas resources, the development characteristics of large-scale high-quality conglomerate reservoirs, the trapping effectiveness of faults, the hydrocarbon migration and accumulation model, and the formation conditions and exploration targets of large- and medium-sized glutenite-rich oil and gas fields. The research results were obtained in four aspects. First, the Paleogene Wenchang Formation in the Huizhou 26 subsag develops extensive and thick high-quality source rocks of semi-deep to deep lacustrine subfacies, which have typical hydrocarbon expulsion characteristics of “great oil generation in the early stage and huge gas expulsion in the late stage”, providing a sufficient material basis for hydrocarbon accumulation in the Enping Formation. Second, under the joint control of the steep slope zone and transition zone of the fault within the sag, the large-scale near-source glutenite reservoirs are highly heterogeneous, with the development scale dominated hierarchically by three factors (favorable facies zone, particle component, and microfracture). The (subaqueous) distributary channels near the fault system, with equal grains, a low mud content (<5%), and a high content of feldspar composition, are conducive to the development of sweet spot reservoirs. Third, the strike-slip pressurization trap covered by stable lake flooding mudstone is a necessary condition for oil and gas preservation, and the NE and nearly EW faults obliquely to the principal stress have the best control on traps. Fourth, the spatiotemporal configuration of high-quality source rocks, fault transport/sealing, and glutenite reservoirs controls the degree of hydrocarbon enrichment. From top to bottom, three hydrocarbon accumulation units, i.e. low-fill zone, transition zone, and high-fill zone, are recognized. The main area of the channel in the nearly pressurized source-connecting fault zone is favorable for large-scale hydrocarbon enrichment. The research results suggest a new direction for the exploration of large-scale glutenite-rich reservoirs in the Enping Formation of the Pearl River Mouth Basin, and present a major breakthrough in oil and gas exploration.

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