基于油田地球物理资料的皮拉拉希油田生产性系列矿床成因与储层物性相互关系研究

IF 0.6 Q4 GEOCHEMISTRY & GEOPHYSICS
K. Kerimova, N.E. Aliyev
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引用次数: 4

摘要

储集岩的岩石物性也受岩石岩性矿物组成与储集物性之间的一定关系的影响。因此,研究生产系列矿床成因与储层物性的关系,为预测整个油田的砂粒分布规律和对孔渗带的发育做出一定的判断提供了依据。这对识别沉积盖层岩石储层物性变化具有重要的科学意义和实际意义。提出了确定沉积岩成因与储层物性关系的合理方法,并对研究结果进行了阐述。作为研究区域,我们选择了位于Pirallahifield同一剖面的常规X1、X2、X3、X4和X5井段研究了“Qirmakiustu粘土”、“Qirmakiustu砂”、“Qirmakiustu系列生产系列沉积物”,并对其沉积环境和相源进行了详细的研究。在研究井段中,有效孔隙度平均值(kv .p.)、砂质层和粘土层平均厚度(h .cl.)在确定流相、坝相和滩平原成因的区间内,计算了砂体(Hrel.sand)的相对厚度。绘制了这些参数在剖面上的变化曲线。同时绘制了各井段确定的层段流相、坝相、滩平原源相厚度曲线。这些曲线分别对每个相进行了比较和分析。研究沉积环境和沉积成因,对比分析岩面物性和储层物性,对准确评价研究区油气存在具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study of the interrelation between the geneseses and reservoir properties of productive series deposits in Pirallahi field on the basis of oil-field geophysical data
Petrophysical properties of reservoir rocks are also influenced by a certain relationship between the lithological-mineralogical composition of rocks and the reservoir properties. For this reason, the study of the relationship between the genesis of Productive Series deposits and reservoir properties provides a basis for predicting the regularity of distribution of sand particles throughout the field and making some judgments about the development of porous and permeability zones. This, in turn, is of more scientific and practical importance while identifying variation of reservoir properties of rocks in sedimentary cover. The paper offers a rational approach that determines the relationship between the genetic origin of sedimentary rocks and their reservoir properties and expounds on the study results. As a research area, we chose «Qirmakiustu clay», «Qirmakiustu sand», Qirmaki and Qirmakialty series of Productive Series sediments studied in sections of conventional X1, X2, X3, X4, and X5 well sections located on one profile of Pirallahifield and their sedimentation environment and facies origin have been studied in more detail. In the section of well under the study, the average value of effective porosity (Kav.p.), average thicknesses of sandy and clayey layers (Hav.cl., Hav.sand), and the relative thickness of sand bodies (Hrel.sand) were calculated for intervals at which the facies of flow, bar, and beach plain origin were identified. The curves of these parameters’ variation across the profile were drawn. At the same time, the curves of thicknesses of flow, bar, and beach plain origin facies were drawn for the interval identified for each well section. These curves were compared and analyzed separately for each facies. A study of the sedimentation environment and genesis of sedimentation and a comparative analysis of lithofacial and reservoir properties may be important for accurately evaluating oil and gas presence in the study area.
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来源期刊
Geofizicheskiy Zhurnal-Geophysical Journal
Geofizicheskiy Zhurnal-Geophysical Journal GEOCHEMISTRY & GEOPHYSICS-
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60.00%
发文量
50
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