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首页> 外文期刊>Petroleum exploration and development >Hydrocarbon charge history of the Tazhong Ordovician reservoirs, Tarim Basin as revealed from an integrated fluid inclusion study
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Hydrocarbon charge history of the Tazhong Ordovician reservoirs, Tarim Basin as revealed from an integrated fluid inclusion study

机译:综合流体包裹体研究揭示塔里木盆地塔中奥陶纪储层的烃充填历史

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This paper presents an integrated workflow for investigating hydrocarbon charge history using fluid inclusions using the Ordovician reservoirs from the Tazhong Oilfield, Tarim Basin as an example. The work flow involves the delineation of fluid inclusion assemblage (FIA) using fluid inclusion petrography and spectroscopy for microthermometric analysis. The interpretation of microthermometric data is based on data derived from synthetic inclusion experiments and takes consideration of the P-T re-equilibration of fluid inclusions in carbonate and over pressure effect on fluid inclusion trapping. The workflow also emphasizes on the requirements of adequate sample preparation, FIA identification, quantitative spectroscopic data (CIE), coeval petroleum and aqueous fluid inclusions, adequate number of microthermometric measurements and integrated interpretation using borehole temperature. In the study reservoirs in the Tazhong area, fluid inclusion spectroscopy reveals the presence of three groups of oil inclusions of near yellow, near blue and near white fluorescence colours. The fluid inclusion microthermometry data indicate the presence of at least two predominant hydrocarbon fluid inclusion assemblages including: homogenous liquid phase yellow fluorescence inclusions and liquid phase oil and condensate fluid inclusion assemblages with homogenous near blue, near white and near yellow fluorescence colours. The aqueous inclusions from the Ordovician reservoirs in the Tazhong area reveal the presence of low, moderate, high and very high salinities in the reservoirs. The extremely high salinity is believed to be caused by regional brine intrusions relating to regional structural movement and deformation.
机译:本文以塔里木盆地塔中油田的奥陶系油藏为例,提出了利用流体包裹体调查烃类充注历史的综合工作流程。工作流程涉及使用流体包裹体岩相学和光谱学进行显微热分析来描述流体包裹体组合(FIA)。微量热测量数据的解释基于合成夹杂物实验得出的数据,并考虑了碳酸盐中流体夹杂物的P-T重新平衡以及过压对流体夹杂物捕集的影响。工作流程还强调了充分样品制备,FIA鉴定,定量光谱数据(CIE),同代石油和含水流体包裹体,足够数量的微热测量和使用井眼温度进行综合解释的要求。在塔中地区的研究油藏中,流体包裹体光谱显示存在三组近黄色,近蓝色和近白色荧光色的油包裹体。流体包裹体显微热力学数据表明存在至少两种主要的烃流体包裹体组合,包括:均相的液相黄色荧光包裹体和液相油和冷凝液流体包裹体组合,具有均一的近蓝色,近白色和近黄色荧光色。塔中地区奥陶系储集层的含水包裹体显示储层中存在低,中,高和非常高的盐度。据认为,极高的盐度是由与区域结构运动和变形有关的区域盐水侵入引起的。

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