塔河油田巴楚组砂砾岩段致密储层成岩作用与孔隙演化

Diagenesis and pore evolution of tight reservoirs in glutenite section of Bachu Formation, Tahe Oilfield

  • 摘要: 石炭系巴楚组砂砾岩段储层致密,是塔河油田未来重要的勘探目的层,但研究非常薄弱,特别是储层成岩作用和孔隙演化不清,严重影响了巴楚组砂砾岩段致密油气的勘探开发。基于巴楚组岩性和沉积相分析,利用岩心、X衍射、铸体薄片、扫描电镜和阴极发光等资料,对塔河油田西部和东部地区巴楚组砂砾岩和砂岩的成岩作用、孔隙演化及其差异进行了系统的研究对比。巴楚组砂砾岩段岩石类型多样,以砂岩和砂砾岩为主,西部地区储层的成分成熟度、结构成熟度、储层物性均高于东部地区。砂砾岩段储层成岩作用以压实作用、胶结作用和溶蚀作用为主,西部地区主要成岩作用为较强的压实作用,强烈的溶蚀作用,中等—较强的胶结作用;东部地区压实作用也较强,而胶结作用更强,溶蚀作用偏弱。结合镜质体反射率、伊蒙混层中蒙脱石的比例以及含铁方解石的出现,认为塔河油田西部和东部地区砂砾岩的成岩阶段均进入中成岩B期。孔隙演化与成岩作用密切相关,西部地区砂岩经过成岩作用,孔隙度由38.8%变为8.8%,砂砾岩孔隙度则由30.5%变为4.5%;东部地区砂砾岩段储层孔隙度经成岩演化由27.0%变为4.0%。该研究可为塔河油田巴楚组砂砾岩段致密油储层评价、勘探开发与甜点优选提供参考。

     

    Abstract: The tight reservoirs in the glutenite section of the Carboniferous Bachu Formation in the Tahe Oilfield represent an important future exploration target. However, research on these reservoirs remains quite limited, particularly regarding diagenesis and pore evolution, which severely restricts the exploration and development of tight oil and gas in the glutenite section of the Bachu Formation. Based on the analysis of lithology and sedimentary facies of the Bachu Formation, this study systematically compared diagenesis, pore evolution, and their differ-ences between glutenite and sandstone in the western and eastern areas of the Tahe Oilfield. The analysis integrated core observations, X-ray diffraction, cast thin sections, scanning electron microscopy, and cathodoluminescence data. The rock types in the glutenite section of the Bachu Formation in Tahe Oilfield were diverse, mainly composed of sandstone and glutenite. The compositional maturity, structural maturity, and physical properties of the reservoirs in the western area were higher than those in the eastern area. Reservoir diagenesis in the glutenite section was mainly characterized by compaction, cementation, and dissolution. In the western area, the main diagenetic processes were strong compaction, intense dissolution, and moderate to strong cementation. In the eastern area, compaction was also strong, cementation was even stronger, but dissolution was relatively weak. Based on vitrinite reflectance (Ro), the proportion of montmorillonite in the mixed layers of illite and montmorillonite, and the occurrence of iron-bearing calcite, it was concluded that the glutenite in both the western and eastern areas of the Tahe Oilfield entered the middle diagenesis stage B. Pore evolution was closely related to diagenesis. In the western area, the porosity of sandstone decreased from 38.8% to 8.8% after diagenesis, while the porosity of glutenite decreased from 30.5% to 4.5%. In the eastern area, the porosity of reservoirs in the glutenite section decreased from 27.0% to 4.0% through diagenetic evolution. This study provides a reference for the evaluation, exploration and development, and sweet spot selection of tight oil reservoirs in the glutenite section of the Bachu Formation in the Tahe Oilfield.

     

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