Changbei gas field is located in Yishan Slope of the northern center of the Ordos Basin,China.The main pay zone reservoir is Upper Paleozoic Lower Permian Shanxi P1S2 quartz arenite,which deposited in distributary channel of delta plain.The reservoir is low porosity low permeability tight reservoir with average porosity of 5.2% and average permeability of 0.7×10-3 μm2 in a current depth of 2 700～2 950 m.Integrated study on depositional environment,lithology,diagenesis and tectonic background has been conducted.The reasons cause this low porosity low permeability tight reservoir features are considered as the following two factors.（1） On one hand,the reservoir was deposited in a coaly bearing acid environment of deltaic distributary channel,the original pore water is acid water with non saturated calcium carbonate,which can not form earlier cementation within the sandstone reservoir.However,compaction has significantly reduce the original pore and pore volume.On the other hand,this acid diagenesis environment cause large amounts of secondary quartz cementation fill the pores left out during compaction of sandstone reservoir.This is the main reasons cause the low porosity low permeability tight reservoir features in the region.Observation from thin section indicate that calcium carbonate cementation is not developed in the pore of sandstone reservoir especially in the earlier stage,the average component of calcium carbonate cementation is 1%～3%,authigenic kaolinite cementation is well developed with an average component of 7%～10%,illite segmentation is also less developed 3%,secondary quartz cementation well develop,mostly reach Ⅱ—Ⅲ level with an average component of 5%～10%,some layer can reach 10%～18% and maximum is 23%,this phenomenon indicated the acid diagenesis environment of P1S2 quartz arenite reservoir in Changbei gas field.（2） Tectonic study indicated that Changbei gas field is located in Ordos Basin tectonically stable at the time when Lower Permian Shanxi Formation was deposited.No tectonic movement and significant structure activities developed so that the formation layers are flat and rare faults and folds seen in the Changbei field.Buried history analysis also indicated that there is no apparently uplift and subsidence after P1S2 Shanxi Formation deposited.Underground water especially organic acid and CO2 acid water is not active,and pore is reduced by compaction and silicon dioxide cementation,acid water can＇t effectively dissolve the reservoir and displacement of materials in the pore.On the other hand,there are few dissolvable components e.g.feldspar（3%）,lithic and carbonate cementation in the rock,hence limited amount of secondary pores generated,this is the second reason that cause poor quality reservoir in Changbei gas field.%长北气田山西组二段主要为三角洲平原分支河道沉积的石英砂岩和岩屑砂岩,其埋藏深度中等（2 700～2 950 m）,但物性较差（孔隙度和渗透率平均分别为5.2%,0.7×10-3μm2）,属于低孔低渗的致密储层。造成低孔低渗的主要原因是：该套砂岩形成于三角洲平原含煤酸性环境,砂岩中原始孔隙水介质呈酸性,碳酸钙处于不饱和状态,难以形成早期碳酸盐胶结,后来埋藏过程中压实作用损失了大量原生孔隙,使得粒间孔隙体积大大减少。同时,酸性成岩环境导致后来压实过程中大规模的石英次生加大,充填砂岩中未被压实损失的残余孔隙,使
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