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Origin and mixing of crude oils in Triassic reservoirs of Mahu slope area in Junggar Basin, NW China: Implication for control on oil distribution in basin having multiple source rocks

机译:西北准Jung尔盆地马湖斜坡区三叠系油藏的原油来源与混合:对多源岩盆地盆地油气分布的控制意义

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The origin of crude oils and their varied geochemical features along the western and northern slope of the Mahu depression in the Junggar Basin has been controversial. Based on the molecular and isotopic geochemistry of hydrocarbons from 46 drill-stem test crude oil samples and 36 core samples, three oil groups (I, II, III) and five subgroups (I-1, I-2, II, III1 and III2) have been recognized and oil-source correlations have been established. The subgroup II oils originated mainly from lower Permian Fengcheng (P(1)f) carbonate source rocks, subgroup I-2 from P(1)f mudstone source rock and group II oils from Middle Permian Wuerhe (P2w) mudstone source rock whose potential was underestimated in the past. Group HI consists of mixed oils, i.e., subgroup IIIl received contributions from P(1)f carbonates and P(2)w mudstones and subgroup III2 is a mixture of oils from Pif mudstones and P(2)w-generated oils. In order to determine the main source rocks, the laboratory oil mixing experiments were carried out. Tricyclic terpane biomarker parameters (lTs) were used to quantify the source contributions. Whole oil carbon isotope ratios were also used to verify the proportions of different oils in each mixture. The results show that subgroup III1 oils have diverse mixing ratios in different reservoir, subgroup III2 oils are mainly from P(1)f mudstones and P(2)w source rock contributes little. Finally, the accumulation process of oil fields along the northern slope of the Mahu depression was analyzed and the contributions from different sources were revealed. This study provides an effective quantitative method to identify contributions from different lacustrine source rocks to mixed oils in the Mahu depression, which could be helpful in predicting location and composition of undiscovered oils. (C) 2016 Elsevier Ltd. All rights reserved.
机译:准gar尔盆地马胡凹陷西部和北部斜坡上的原油来源及其变化的地球化学特征一直引起争议。基于46个钻杆测试原油样品和36个岩心样品中烃的分子和同位素地球化学特征,三个油类(I,II,III)和五个亚组(I-1,I-2,II,III1和III2) )已被识别,并且已建立了油源相关性。 II组油主要来自下二叠系凤城(P(1)f)碳酸盐岩,I-2组来自P(1)f泥岩源岩和II组来自中二叠系乌尔河(P2w)泥岩源岩在过去被低估了。 HI组由混合油组成,即,IIIl子组从P(1)f碳酸盐和P(2)w泥岩中得到贡献,而III2子组是Pif泥岩和P(2)w生成的油的混合物。为了确定主要烃源岩,进行了实验室油混合实验。三环萜类生物标志物参数(lTs)用于量化来源贡献。全油碳同位素比也用于验证每种混合物中不同油的比例。结果表明,Ⅲ1类油在不同的储层中具有不同的混合比,Ⅲ2类油主要来自P(1)f泥岩,P(2)w烃源岩贡献不大。最后,分析了马湖depression陷北坡油田的成藏过程,揭示了不同来源的贡献。这项研究提供了一种有效的定量方法,可识别出不同湖相烃源岩对麻湖depression陷混合油的贡献,这可能有助于预测未发现油的位置和组成。 (C)2016 Elsevier Ltd.保留所有权利。

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