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Main controlling factors and distribution of high quality reservoirs of deep buried dolomite in typical craton basins in China

Zhang Jian-yong1,2,Ni Xin-feng1,2,Wu Xing-ning1, Li Wen-zheng1,Hao Yi1,Chen Ya-na1,Lü Xue-ju1,Gu Ming-feng1,Tian Han1,Zhu Mao1   

  1. 1.PetroChina Hangzhou Research Institute of Geology,Hangzhou 310023,China;2.CNPC Key Lab of Carbonate Reservoir,Hangzhou 310023,China
  • Received:2017-05-26 Revised:2017-07-11 Online:2017-08-10 Published:2017-08-10

Abstract:

Deep dolomite in craton basin is an important field for future natural gas exploration in China.Through statistical analysis,it is clear that the main types of deep dolomite are granular dolomite,microbial dolomite and crystalline dolomite,the pore types are mainly fractured fissure cavity and fractured pore type.It is pointed out that favorable sedimentary microfacies are the material basis for pore formation,early dissolution is a necessary condition for pore formation,dolomitization is beneficial to preservation of early pores,epigenetic karstification and structural fracture improve reservoir property.Definite,the deep quality dolomite reservoirs are still facies controlled,the deep dolomite reservoir is more inherited than transformed,the vertical distribution is not controlled by depth,but controlled by early sedimentary cycles,the lateral distribution is not controlled by karstification,but controlled by high-energy sedimentary facies belts.It is considered that the exploration of deep quality dolomite reservoirs in the future will be mainly “both sides of the inner rift of platform” and carbonate ramps.

Key words: Craton basin, Deep layers, Dolomite reservoir, Sichuan Basin, Tarim Basin, Ordos Basin

CLC Number: 

  • TE122.2

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