有机地球化学在烃源岩储层勘探中的应用综述

Joseph A. Curiale , John B. Curtis
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引用次数: 70

摘要

烃源岩储层是细粒烃源岩,裂缝改造后可产出液态和气态烃。使这种烃源岩能够很好地发挥储层作用的一个主要因素是它的有机质——特别是在烃源岩储层中出现的有机质的数量、质量和热成熟度。在此,我们回顾了已发表的文献,对这些储层中有机质的地球化学测量和数据解释的现状进行了评价,以及工作人员如何将这些信息应用于该储层类型的勘探。我们的研究重点是烃源岩储层的化学和地球化学特征,重点是烃流体和固体有机质的同位素和分子特征。特别考虑了特别适用于该储层类型有机质的地球化学分析方法。我们对已发表研究的讨论集中在三个方面:(a)烃源岩特征——有机质数量、质量和成熟度;(b)干酪根、石油、凝析油和天然气的热致裂解;(3)页岩储层天然气稳定碳同位素异常。概念方法和实际应用在同等程度上进行了讨论,并提供了我们对未来方向和未解决问题的评估。
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Organic geochemical applications to the exploration for source-rock reservoirs – A review

Source-rock reservoirs are fine-grained petroleum source rocks from which liquid and gaseous hydrocarbons may be produced following fracture stimulation. A major factor that allows such a source rock to function well as a reservoir is its organic matter – specifically the quantity, quality and thermal maturity of that organic matter as it occurs within the source-rock reservoir. Here we review the published literature to assess the current status of geochemical measurement and data interpretation of organic matter in these reservoirs, and how workers have applied this information in the exploration for this reservoir type. Our focus is on the chemical and geochemical characteristics of source-rock reservoirs, with emphasis on the isotopic and molecular characteristics of their hydrocarbon fluids and solid organic matter. Special consideration is given to geochemical analytical methods particularly appropriate to the organic matter in this reservoir type. Our discussions of published studies focus on three areas: (a) source rock characteristics – organic matter quantity, quality and maturity; (b) thermally-induced cracking of kerogen, oil, condensate and gas; and (c) natural gas stable carbon isotopic anomalies often observed in shale plays. Conceptual approaches and practical applications are addressed in equal measure, and our assessment of future directions and unsolved problems is provided.

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