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Brittleness index estimation in a tight shaly sandstone reservoir using well logs

机译:利用测井曲线估算致密页岩砂岩储层的脆性指数

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Premise evaluation of the ability of fracture network forming using hydraulic fracturing is crucial for the development of tight shaly sandstone reservoirs. X-ray diffraction, petrographic analysis integrated with petrophysical well logs was used to provide insights to the brittleness of Chang 7 shaly sandstone in the Ordos basin. The mineralogical composition of this unit is quartz, clay, carbonates and feldspar with minor quantities of pyrite. Quartz and carbonate are the critical brittle minerals. The brittleness index defined in terms of mineralogy and geomechanical properties was investigated respectively. The geomechanical brittleness derived from dipole acoustic logs has a wide range from 0.98% to 93.21%, averaging 58.07%. In contrast, the mineralogical brittleness index from X-ray diffraction results is in the range of 28.26-78.85%, averaging 59.31%. The geomechanical brittleness index could be easily calculated using the dipole acoustic and bulk density logs. For wells without dipole acoustic logs, predicting the brittleness index using conventional well log suits is of great importance. The mineralogical brittleness index was then correlated with their well-log signatures. Statistical regression analysis was carried out to find the relations between brittleness index and conventional well logs, and it is found that the ratio of gamma ray to photoelectric absorption cross section index (GR/Pe) shows a good correlation with brittleness index. Therefore, the brittleness index could be estimated using conventional logs (GR/Pe). The geomechanical brittleness index and the test oil results confirm the reliability of the brittleness index estimation model. Favorable layers for hydraulic fracturing are mainly associated with the intervals with high values of brittleness index. This work is valuable for the evaluation of hydraulic fracturing effects in unconventional oil and gas reservoirs in the future. (C) 2015 Elsevier B.V. All rights reserved.
机译:对水力压裂裂缝网络形成能力的前提评估对于致密的泥质砂岩储层的开发至关重要。 X射线衍射,岩石学分析与岩石物理测井相结合,被用来洞察鄂尔多斯盆地长7泥质砂岩的脆性。该单元的矿物学组成是石英,粘土,碳酸盐和长石,以及少量的黄铁矿。石英和碳酸盐是重要的脆性矿物。分别研究了根据矿物学和地质力学性质定义的脆性指数。由偶极声波测井仪得出的地质力学脆性范围从0.98%到93.21%,平均为58.07%。相反,X射线衍射结果的矿物学脆性指数在28.26-78.85%的范围内,平均为59.31%。使用偶极声波和堆积密度测井曲线可以很容易地计算出地质力学的脆性指数。对于没有偶极声测井的井,使用常规测井服预测脆性指数非常重要。然后将矿物学脆性指数与其测井特征联系起来。通过统计回归分析发现了脆性指数与常规测井曲线之间的关系,发现γ射线与光电吸收截面指数的比值(GR / Pe)与脆性指数具有良好的相关性。因此,可以使用常规测井仪(GR / Pe)估算脆性指数。地质力学脆性指数和试油结果证实了脆性指数估算模型的可靠性。水力压裂的有利层主要与脆性指数高的区间有关。这项工作对于未来非常规油气藏的水力压裂效果评估具有重要意义。 (C)2015 Elsevier B.V.保留所有权利。

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