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- W2384153158 abstract "Based on analyzing some experimental materials of the Jurassic tight sandstone reservoirs,such as ordinary slice,casting slice,mercury injection curves,in Jiulongshan Region on the northern margin of the Qaidam Basin,it can be found that lithic sandstones and feldspathic lithic sandstone were the main types of rock,debris-arkosic sandstone and feldspathic sandstone were also included.Interparticle dissolution pore was the main type of pore,and residual intergranular pore and intragranular dissolved pore were the secondary type.The average porosity and permeability was 9.07%and 1.71×10-3μm2,respectively,so the Jurassic tight sandstone reservoirs in Jiulongshan Region belonged to the typical low-porosity and ultra lowpermeability reservoirs.Through Microscopic identification and electron microscopy scanning,there were four kinds of carbonate cements:calcite,iron-bearing calcite,dolomite and ankerite,and the clay minerals were dominated by illite,chlorite and illite smectite mixed layer.The particles of tight sandstone reservoirs were fine with poor sorting and low psephicity.Lithic sandstones and feldspathic lithic sandstone were the main types of rock,and lithic component were mainly the plastic rock which has low anti-compaction,which mainly controlled the formation of the tight sandstone reservoirs.Secondly,the Jurassic reservoirs were buried deeply,and strong compaction made their porosity and permeability reduced.In later stage,the dissolution of carbonate cements and soluble particles improved the porosity and permeability." @default.
- W2384153158 created "2016-06-24" @default.
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- W2384153158 date "2014-01-01" @default.
- W2384153158 modified "2023-09-28" @default.
- W2384153158 title "Genesis of Jurassic Tight Sandstone Reservoirs of Jiulongshan Region in the Northern Qaidam Basin" @default.
- W2384153158 hasPublicationYear "2014" @default.
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