构造-热液过程及其与西西伯利亚巴热诺夫-阿巴拉克复合体石油潜力的关系

M. Yu. Zubkov
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引用次数: 0

摘要

--在巴热诺夫-阿巴拉克复合地层中已经确定了储层岩石的主要类型。为了评估碳氢化合物的地质资源,建议将巴热诺夫-阿巴拉克岩群的所有岩性划分为两大类:流体封存和储层。我们认为,根据测井数据,可以区分潜在富集岩和富集岩(以硅质岩和碳酸盐岩为代表)。我们重建了巴热诺夫-阿巴拉克复合地层中储层岩石的可能形成机制,这是构造-热液对这些矿床影响的结果。通过整合地震数据和在其基础上进行的构造物理建模,提出了确定巴热诺夫-阿巴拉克复合地层中各类碳氢化合物积聚远景区的独创方法。例如,在叶姆-叶戈夫斯卡娅地区的三维地震勘探范围内,对巴热诺夫-阿巴拉克综合体所含碳氢化合物的预测地质资源进行了评估。根据整个巴热诺夫-阿巴拉克复合地层(而不仅仅是巴热诺夫地层)中构造-热液成因储层岩石的单一形成机制,证实了评估石油含量前景和计算碳氢化合物预测地质资源量的必要性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Tectonic–Hydrothermal Processes and their Relationship with the Petroleum Potential of the Bazhenov-Abalak Complex of Western Siberia
––The main types of reservoir rocks have been identified within the Bazhenov-Abalak complex. To assess the geological resources of hydrocarbons, it is proposed to formally divide the entire set of lithological rock types comprising the Bazhenov-Abalak complex into two main varieties: fluid seals and reservoirs. We argue that it is possibile to distinguish between potentially productive and productive rocks, represented by siliceous and carbonate varieties, according to logging data. A possible mechanism for the formation of reservoir rocks within the Bazhenov-Abalak complex as a result of the tectonic-hydrothermal impact on these deposits has been reconstructed. An original methodology for identifying perspective zones of various categories of hydrocarbon accumulation in the Bazhenov-Abalak complex through integrating seismic data and tectonophysical modeling carried out on their basis has been proposed. For example, an assessment of the predicted geological resources of hydrocarbons contained in the Bazhenov-Abalak complex within the limits of 3D seismic exploration of the Yem-Yegovskaya area has been carried out. The necessity of assessing the prospects for oil content and calculating the predicted geological resources of hydrocarbons in the whole Bazhenov-Abalak complex, and not only in the Bazhenov Formation, is substantiated, based on a single mechanism of formation of reservoir rocks of tectonic-hydrothermal origin in them.
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