Clumped isotope,Carbonate reservoirs,Temperature,Fluid properties,Diagenesis,"/> The implication and significance of clumped isotope in carbonate reservoirs

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The implication and significance of clumped isotope in carbonate reservoirs

Hu An-ping,Shen An-jiang,Pan Li-yin,Wang Yong-sheng,Li Xian-jing,Wei Dong-xiao   

  1. 1.PetroChina Hangzhou Research Institute of Geology,Hnagzhou 310023,China;
    2.CNPC Key Laboratory of Carbonate Reservoirs,Hangzhou 310023,China
  • Received:2017-07-24 Revised:2017-12-01 Online:2018-01-10 Published:2018-01-10

Abstract:

Carbonate clumped isotope has become a new kind of carbonate thermometry in recent years.After calculated from clumped isotope,the carbonate formation temperature and the oxygen isotope of the diagenetic fluids could be derived,which are of great significance to the study of diagenetic environment of carbonate reservoirs.Three kinds of typical carbonates were collected for clumped isotope and other elements isotope study,to conclude the implication of clumped isotope in the carbonate reservoirs diagenesis:①for simple samples without complex diagenetic modification,the clumped isotope and its calculated results directly indicate the temperature and fluid properties of the diagenetic environment;②for the samples only influenced by burial high temperature,the clumped isotope temperature might change and reflect the burial environment,but the oxygen isotope unchanged and indicated the original forming environment;③for the samples obviously reformed by post-diagenesis due to post-fluid entering,the clumped isotope temperature and oxygen isotope of the fluid will change in both calcite and dolomite,indicating the mixed result of the carbonate formation environment and post-diagenetic environment.
 

Key words: Clumped isotope')">

CLC Number: 

  • TE122
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