澳大利亚西北部Vulcan亚盆地页岩砂储层岩石物性参数对比分析

Ulrike Johanna, Epo Prasetya Kusumah
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引用次数: 0

摘要

Vulcan次盆地位于澳大利亚西北部的Bonaparte盆地,是一个油气勘探非常丰富的地区。通过电阻率测井和密度测井的筛选,确定了一些含粘土的砂岩储层,通常称为泥质砂岩储层。粘土含量导致泥质砂岩储层电阻率测井读数较低,因此认为泥质砂岩储层为非储层。为了克服这一问题,在常规方法的基础上,提出了一种分析泥质砂岩储层岩石物性参数的方法——泥质砂岩法。岩石物理分析是根据测井资料对页岩体积、孔隙度、含水饱和度等岩石物理参数进行分析。本研究利用35口测井资料,包括伽马测井、电阻率测井、中子测井、密度测井等,对Vulcan子盆地进行了岩石物理分析,其中常规方法和页岩砂法采用了Stieber方程和Thomas Stieber图。研究结果是常规方法与页岩砂法的岩石物性参数值和储层概况的比较,以及与页岩分布类型的关系。应用泥质砂法后,页岩平均体积减小,平均孔隙度增大,平均含水饱和度增大,平均净重比增大,平均净厚度增大,平均净产层增加。平均值的变化主要是受成岩作用和地层沉积环境影响的层状-分散页岩分布类型所致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analysis of Petrophysical Parameter on Shaly Sand Reservoir by Comparing Conventional Method and Shaly Sand Method in Vulcan Subbasin, Northwest Australia
Vulcan Subbasin is an area with a lot of oil and gas exploration where is located in the Bonaparte Basin, Northwest Australia. There is some formation identified as sandstone reservoir with clay content which is usually called shaly sand based on the screening between resistivity log and density log. Clay content caused lower resistivity log readings so the shaly sand reservoir is considered as non-reservoir. To overcome this, a method besides the conventional method was applied to analyze the petrophysical parameters of shaly sand reservoir, it was shaly sand method. Petrophysical analysis is an analysis of rock physical parameters such as shale volume, porosity, and water saturation based on well log data. In this study, petrophysical analysis was carried out in the Vulcan Subbasin using 35 well log data, including gamma ray log, resistivity log, neutron log, and density log for the conventional method and shaly sand method involved Stieber equation and Thomas Stieber plot. The results obtained from this study are the comparison of petrophysical parameter values and pay summary between the conventional method and the shaly sand method, also its relation to the shale distribution type. By applying the shaly sand method, the average shale volume has decreased, the average porosity has increased, the average water saturation has increased, the average net to gross has increased, the average net thickness has increased, and the average net pay has increased. Changes in the average value were caused by laminated-dispersed shale distribution type which is influenced by diagenesis and the depositional environment of the formation.
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