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首页> 外文期刊>Current Organic Synthesis >Light hydrocarbon geochemistry: insight into oils/condensates families and inferred source rocks of the Woodford-Mississippian tight oil play in North-Central Oklahoma, USA
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Light hydrocarbon geochemistry: insight into oils/condensates families and inferred source rocks of the Woodford-Mississippian tight oil play in North-Central Oklahoma, USA

机译:轻质碳氢化合物地球化学:洞察油/凝聚体家庭,并在美国北部俄克拉荷马州北部的伍德福德密西西比酒剧本的推断源岩

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The Woodford-Mississippian "Commingled Production" is a prolific unconventional hydrocarbon play in Oklahoma, USA. The tight reservoirs feature variations in produced fluid chemistry usually explained by different possible source rocks. Such chemical variations are regularly obtained from bulk, molecular, and isotopic characteristics. In this study, we present a new geochemical investigation of gasoline range hydrocarbons, biomarkers, and diamondoids in oils from Mississippian carbonate and Woodford Shale. A set of oil/condensate samples were examined using high-performance gas chromatography and mass spectrometry. The result of the condensates from the Anadarko Basin shows a distinct geochemical fingerprint reflected in light hydrocarbon characterized by heptane star diagrams, convinced by biomarker characteristics and diamantane isomeric distributions. Two possible source rocks were identified, the Woodford Shale and Mississippian mudrocks, with a variable degree of mixing. Thermal maturity based on light hydrocarbon parameters indicates that condensates from the Anadarko Basin are of the highest maturity, followed by "Old" Woodford-sourced oils and central Oklahoma tight oils. These geochemical parameters shed light on petroleum migration within Devonian-Mississippian petroleum systems and mitigate geological risk in exploring and developing petroleum reservoirs.
机译:Woodford-Mississippian“混合制作”是美国俄克拉荷马州的一种多产的不传统碳氢化合物。紧密的水库特征在产生的流体化学中的变化通常由不同的可能的源极岩解释。这些化学变化经常从散装,分子和同位素特征中获得。在这项研究中,我们展示了Mississippian碳酸盐和伍德福德页岩油的汽油系列烃类碳氢化合物,生物标志物和表情的新地球化学研究。使用高性能气相色谱和质谱法检测一组油/冷凝物样品。来自Anadarko盆地的冷凝物的结果显示了一种不同的地球化学指纹,其在以庚烷星形图为特征在于庚烷星形图,通过生物标志物特性和二氨基甲烷异构分布来说服。识别出两块可能的源岩,伍德福德页岩和密西西比泥屑,具有可变的混合程度。基于轻质烃参数的热成熟表示,Anadarko盆地的冷凝物是最高成熟度,其次是“旧”伍德福德 - 源油和中央俄克拉荷马州紧密油。这些地球化学参数揭示了德文郡 - 密西西比石油系统内的石油迁移,并减轻了探索和发展石油储层的地质风险。

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