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Structure and Filling Characteristics of Paleokarst Reservoirs in the Northern Tarim Basin, Revealed by Outcrop, Core and Borehole Images

机译:塔里木盆地北部古岩溶储层的结构和充填特征,通过露头,岩心和钻孔图像显示

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The Ordovician paleokarst reservoirs in the Tahe oilfield, with burial depths of over 5300 m, experienced multiple phases of geologic processes and exhibit strong heterogeneity. Core testing can be used to analyse the characteristics of typical points at the centimetre scale, and seismic datasets can reveal the macroscopic outlines of reservoirs at the 10-m scale. However, neither method can identify caves, cave fills and fractures at the meter scale. Guided by outcrop investigations and calibrations based on core sample observations, this paper describes the interpretation of high longitudinal resolution borehole images, the identification of the characteristics of caves, cave fills (sedimentary, breccia and chemical fills) and fractures in single wells, and the identification of structures and fill characteristics at the meter scale in the strongly heterogeneous paleokarst reservoirs. The paleogeomorphology, a major controlling factor in the distribution of paleokarst reservoirs, was also analysed. The results show that one well can penetrate multiple cave layers of various sizes and that the caves are filled with multiple types of fill. The paleogeomorphology can be divided into highlands, slopes and depressions, which controlled the structure and fill characteristics of the paleokarst reservoirs. The results of this study can provide fundamental meter-scale datasets for interpreting detailed geologic features of deeply buried paleocaves, can be used to connect core- and seismic-scale interpretations, and can provide support for the recognition and development of these strongly heterogeneous reservoirs.
机译:塔河油田奥陶系古喀斯特储层埋藏深度超过5300 m,经历了多个地质过程阶段,表现出较强的非均质性。岩心测试可以用来分析厘米级典型点的特征,地震数据集可以揭示大于10米规模的油藏的宏观轮廓。但是,两种方法都无法在米级上识别洞穴,洞穴填充物和裂缝。在基于岩心样本观测资料的露头调查和标定的指导下,本文描述了高纵向分辨率井眼图像的解释,洞穴特征,洞穴填充物(沉积,角砾岩和化学填充物)和单井裂缝的识别,以及高度异质的古喀斯特储层的米级结构和填充特征的识别。还分析了古地貌,这是古喀斯特储层分布的主要控制因素。结果表明,一口井可以穿透多个大小各异的溶洞层,并且这些溶洞充满了多种填充物。古地貌可分为高地,斜坡和洼地,它们控制了古喀斯特储层的结构和充填特征。这项研究的结果可以为解释深埋古洞穴的详细地质特征提供基础的米级数据集,可以用来连接岩心级和地震级解释,并可以为这些强非均质油藏的识别和开发提供支持。

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