咸化湖盆细粒混合层序油气成藏关键控制因素——青藏高原柴达木盆地西北部含油气系统综合研究

IF 4.8 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Dehao Feng, Chenglin Liu, Jixian Tian, Minjunshi Xie, Hongliang Huo, Taozheng Yang, Guoxiong Li, Yubo He
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引用次数: 0

摘要

盐湖环境中形成的细粒碳酸盐-硅屑混合层序构成了大量非常规和常规油气资源。明确油气成藏的关键控制因素,是预测潜在资源和完善勘探策略的关键。然而,对于油气如何在细粒碳酸盐-硅-塑性混合层序中富集,目前还缺乏研究。在地球化学分析、储层资料、流体包裹体分析和盆地模拟等基础上,对柴达木盆地西北部独特的含盐湖相含油气系统进行了综合研究。咸化湖相烃源岩有机质丰度较低,有机质类型为II-III型。盐化湖相烃源岩可溶有机质含量高,烃源岩厚度大,为含油气系统提供了充足的烃源岩。储层岩石表现出不同寻常的碳酸盐和硅质矿物混合特征。溶蚀和微裂缝发育是形成优质储层的关键。中新世中期油气充注开始,主要发生在早期圈闭形成的地区。晚中新世-上新世晚期圈闭开始充注油气。咸化湖盆油气成藏的关键控制因素包括:(1)充足的油气供应;(2)优质的细粒混合储层;(3)有利的生储盖组合;(4)湖盆中部构造运动形成的大量背斜圈闭;(5)地质要素匹配关系适宜。建立了早期圈闭和晚期圈闭的油气成藏模式,为今后的勘探奠定了基础。该研究为盐化湖相含油气系统提供了新的认识,可为今后全球其他盐化湖相盆地的油气勘探提供有效模板。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Key Controlling Factors of Hydrocarbon Accumulation of Fine-Grained Mixed Sequence in a Saline Lacustrine Basin: An Integrated Research of Petroleum System in the Northwestern Qaidam Basin, Qinghai–Tibet Plateau

Fine-grained carbonate-siliciclastic mixed sequences, formed in saline lacustrine settings, constitute substantial unconventional and conventional hydrocarbon resources. Clarifying the key controlling factors of hydrocarbon accumulation is pivotal for predicting potential resources and enhancing exploration strategies. However, there is still a lack of research on how hydrocarbons accumulate in fine-grained carbonate-siliciclastic mixed sequences. Here, we present integrated research on a unique saline lacustrine petroleum system with fine-grained mixed deposits in the northwestern Qaidam Basin based on geochemical analysis, reservoir data, fluid inclusion analysis, and basin modeling. The saline lacustrine source rocks have low organic abundance, with type II–III organic matter. The high content of soluble organic matter and large thickness of saline lacustrine source rock provided sufficient hydrocarbon for the petroleum system. The reservoir rocks exhibit unusual mixed characteristics of carbonate and siliceous minerals. Dissolution and microfracture development are critical for the formation of high-quality reservoirs. Hydrocarbon charging began during the Middle Miocene, and initially, it occurred in those areas where early traps were formed. By comparison, hydrocarbon began to charge late traps during the Late Miocene or Pliocene. The crucial controlling factors of hydrocarbon accumulation in the saline lacustrine basin include (1) adequate hydrocarbon supply, (2) high-quality fine-grained mixed reservoirs, (3) favorable source–reservoir–caprock assemblage, (4) many anticlinal traps generated by tectonic movements in the central lacustrine basin, and (5) suitable matching relationship of geological elements. This research also established hydrocarbon accumulation models of early trap and late trap to promote future exploration. This research provides new insights into a saline lacustrine petroleum system, which may serve as an efficient template for other saline lacustrine basins worldwide to promote future petroleum exploration.

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来源期刊
Natural Resources Research
Natural Resources Research Environmental Science-General Environmental Science
CiteScore
11.90
自引率
11.10%
发文量
151
期刊介绍: This journal publishes quantitative studies of natural (mainly but not limited to mineral) resources exploration, evaluation and exploitation, including environmental and risk-related aspects. Typical articles use geoscientific data or analyses to assess, test, or compare resource-related aspects. NRR covers a wide variety of resources including minerals, coal, hydrocarbon, geothermal, water, and vegetation. Case studies are welcome.
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