The reservoirs in Xujiahe formation of Chuanxi depression are tight sandstones with low permeability.
川西须家河组储层为低渗超致密储层,使传统的测井解释技术在多方面受到限制.
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The groundwater of Xujiahe formation is mainly the calcium chloride type of gas field water.
须家河组地层水主要为氯化钙型的气田地层水.
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Xujiahe Formation reservoir is the typical tight sandstone in transitional zone of middle - south Sichuan.
四川盆地川中 — 川南过渡带须家河组为典型的致密化砂岩储层.
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