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首页> 外文期刊>Marine and Petroleum Geology >Multiple-stage migration and accumulation of Permian lacustrine mixed oils in the central Junggar Basin (NW China)
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Multiple-stage migration and accumulation of Permian lacustrine mixed oils in the central Junggar Basin (NW China)

机译:准gar尔盆地中部(中国西北)二叠纪湖相混合油的多阶段运移和聚集

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The Permian lacustrine petroleum system in the central Junggar Basin, northwest China, has recently obtained exploration success. These accumulations are characterized by mixed oils and multiple-stage migration and accumulation. This process, however, has not been well constrained, limiting the understanding of the general laws of hydrocarbon migration and accumulation and making it difficult to define exploration strategies. Here, we reconstruct this process mainly based on oil-bearing fluid inclusion analyses including petrography, homogenization temperature and sequential extraction. Inclusion petrography shows that petroleum inclusions dominantly display yellow fluorescence, while intergranular free oils mostly display strong blue green fluorescence. This implies that the reservoirs seem to have experienced at least two stages of hydrocarbon charge from different sources and/or maturities. The sources/maturities are determined through reservoir sequential extraction analyses. The free oils are mixed and sourced from the Lower Permian Fengcheng Formation (P(1)f) and the Middle Permian Lower Wuerhe Formation (P(2)w), while the inclusion oils are also mixed and derived mainly from the P(1)f source. Both oils are characterized by moderate maturity. Homogenization temperature measurements of oil-bearing fluid inclusions, combined with reconstruction of reservoir burial and thermal history, not only further verify multiple hydrocarbon charging events but also characterize the timing, which indicates a three-stage petroleum charging model. During the first stage of the Late Triassic, Carboniferous reservoirs were charged by P(1)f-sourced oils, which were dysmigrated or remigrated to Jurassic reservoirs during the second stage (i.e., the Early Cretaceous). In contrast, the third stage from the Late Cretaceous represents another hydrocarbon charge event that is the primary oil accumulation sourced from the P2w rocks. According to this model, both primary and secondary oil accumulations contribute to the current region's exploration success, and provide future exploration targets. (C) 2014 Elsevier Ltd. All rights reserved.
机译:中国西北准Jung尔盆地中部的二叠纪湖相石油系统最近获得了勘探成功。这些堆积物的特征是混合油和多阶段运移和堆积。但是,这个过程并没有得到很好的约束,这限制了人们对烃类运移和聚集的一般规律的理解,并且难以确定勘探策略。在此,我们主要基于含油流体包裹体分析(包括岩相学,均质温度和顺序提取)来重构此过程。包裹体岩相学表明,石油包裹体主要显示黄色荧光,而粒间游离油则大多显示强蓝绿色荧光。这暗示着储层似乎经历了来自不同来源和/或成熟度的至少两个阶段的烃充注。来源/成熟度是通过储层相继提取分析确定的。游离油是从下二叠系凤城组(P(1)f)和中二叠统下乌尔河组(P(2)w)混合而来的,而夹杂油也被混合且主要来自P(1) )f来源。两种油均具有适度的成熟度。含油流体包裹体的均质温度测量,再结合储层埋藏和热历史,不仅进一步验证了多个烃类充注事件,而且表征了时机特征,这表明了一个三阶段石油充注模型。在晚三叠世的第一阶段,石炭系储层由P(1)f来源的油充注,这些油在第二阶段(即白垩纪早期)被迁移或迁移到侏罗纪储层。相比之下,白垩纪晚期的第三阶段代表了另一个烃类充注事件,这是从P2w岩石中获取的主要油藏。根据该模型,初级和次级油藏都有助于当前地区的勘探成功,并提供未来的勘探目标。 (C)2014 Elsevier Ltd.保留所有权利。

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