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The Physical Properties and Their Prediction of Volcanic Reservoirs in Luxi Area of Junggar Basin, China

机译:中国准噶尔盆地鲁西地区火山水库的物理性质及其预测

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The physical properties of reservoirs determine the ability on accumulating hydrocarbon. As one of the unconventional hydrocarbon reservoirs, the volcanics own the different characteristics from the clastic rocks on physical properties. The study on the relationship between physical and electrical properties of deep volcanic reservoirs was conducted, using the Luxi area of Junggar basin as an example. By our study, some conclusions have been made: The heterogeneity of physical properties is strong in volcanic rocks whose porosity and permeability vary in different lithology and lithofacies; different rocks in a same well have various values of porosity and permeability, and a certain type of volcanic rock has different values of porosity and permeability in diverse wells. According to measured data, the value of porosity an permeability in erupting and effusive facies area are high, while in volcanic channel and extrusive facies as well as volcanic sedimentation facies are low. Unlike the clastic rocks, in volcanic rocks there is little relationship between porosity and permeability and all of them do not have close relationship to the buried depth. Different electrical responses have different relationship with the porosity of one certain lithology, while one certain electrical property has different responses for the porosities of different lithologies; comparatively speaking, the porosities of tuffites, breccia correlate intensively with GR, SP and AC, so these electrical parameters can be utilized to predict the physical properties. This study illustrated that the relativities between porosity and GR, AC, and SP are Por=-0.6189×GR+52.691 (R~2=0.9311), Por =-0.3771×AC + 34.5 (R~2=0.8876) and Por = 2.1458×SP + 79.404 (R~2=0.8236).
机译:储层的物理性质决定了积累烃的能力。作为一个非传统的碳氢化合物储层之一,火山虫拥有从物理性质的碎片岩石中的不同特征。对深火山水库物理和电学性质关系的研究是在Junggar盆地的鲁西地区进行的。通过我们的研究,已经进行了一些结论:物理性质的异质性在火山岩中强大,其孔隙率和渗透率不同于不同的岩性和锂缺陷;同样良好的不同岩石具有各种孔隙率和渗透性的值,并且某种类型的火山岩具有不同的孔隙率和不同孔的渗透值。根据测量数据,孔隙率的价值爆发和活化相面积的渗透性高,而在火山通道和喷射相以及火山沉降相位低。与碎片岩石不同,在火山岩中,孔隙率和渗透性之间的关系很小,并且所有这些都没有与埋藏深度密切相关的关系。不同的电反应与一定岩性的孔隙率不同,而某种电性能对不同岩性的孔隙率有不同的反应;相对言,牙龈细胞的孔隙率,Breccia与GR,SP和AC强烈地相关,因此这些电气参数可用于预测物理性质。本研究说明孔隙率和GR,AC和SP之间的相对性是POR = -0.6189×GR + 52.691(R〜2 = 0.9311),POR = -0.3771×AC + 34.5(R〜2 = 0.8876)和POR = 2.1458×SP + 79.404(R〜2 = 0.8236)。

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