Zhou Chaoran, Shao Junlin. THE BEHAVIOR OF LOWER PALEOZOIC CAR-BONATE RESERVOIR IN LAIWU AREA SOUTHWESTERN SHANDONG[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1985, 7(2): 148-154. doi: 10.11781/sysydz198502148
Citation: Zhou Chaoran, Shao Junlin. THE BEHAVIOR OF LOWER PALEOZOIC CAR-BONATE RESERVOIR IN LAIWU AREA SOUTHWESTERN SHANDONG[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1985, 7(2): 148-154. doi: 10.11781/sysydz198502148

THE BEHAVIOR OF LOWER PALEOZOIC CAR-BONATE RESERVOIR IN LAIWU AREA SOUTHWESTERN SHANDONG

doi: 10.11781/sysydz198502148
  • Received Date: 1984-03-01
  • Publish Date: 1985-04-25
  • The behavior of Paleozoic carbonate reservoir in Laiwu area is roughly known by pore geometry analysis,thin section cast observation and conventional petro-physical properties determination.There are more than 20 layers with thickness of 150m are favourable reservoir in this section.The types of the reservoir are:for Middle Cambrian,mainly dissolution vug type;for Ordovician,mainly fracture-dissolution vug type.There are 12 types of pore space:dissolution pore;intercrystalline pore;intercrystalline dissolution pore;intracrystalline dissolution pore;intergranular dissolution pore;intragranular dissolution pore;dolomite casting mould pore;structural fracture;interformational fracture;diagenetic fraccture;dissolution trace,stylolite etc.Secondary pore zones with developed dissolution pore,cavern,and crack were often formed near paleoerosional surfaces.There sre 6 secondary pore zones in this section.

     

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