The Shan1 He8 Member is tight sandstone with many consedimental volcanics in the middle-north of Ordos Basin.
Compared with common clastic rocks,the fillings of tight sandstone are of many types,complicated components,and intensive
diagenetic evolution. The fillings consist of consedimental volcanic ash,clay mineral,carbonate cement and metasome,
siliceous cement,slender glimmer,muddy debris and carbon dust. Based on the research of reservoirs,the relativity of the
fillings and pore evolution was studied by using slices,scanning electron microscopy,cathode luminescence and so on. The
analysis is mainly focused on genesis,character,diagenetic evolution of fillings. Research shows that consedimental volcanic
ash is mother material of secondary dissolved pores;calcite cement strongly damage pore in late-diagenetic period,and certain
amount of kaolinite is favorable for pore growing.