Volume 41 Issue 3
Mar.  2016
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Yu Zhichao, Liu Keyu, Zhao Mengjun, Liu Shaobo, Zhuo Qingong, Lu Xuesong, 2016. Characterization of Diagenesis and the Petroleum Charge in Kela 2 Gas Field, Kuqa Depression, Tarim Basin. Earth Science, 41(3): 533-545. doi: 10.3799/dqkx.2016.044
Citation: Yu Zhichao, Liu Keyu, Zhao Mengjun, Liu Shaobo, Zhuo Qingong, Lu Xuesong, 2016. Characterization of Diagenesis and the Petroleum Charge in Kela 2 Gas Field, Kuqa Depression, Tarim Basin. Earth Science, 41(3): 533-545. doi: 10.3799/dqkx.2016.044

Characterization of Diagenesis and the Petroleum Charge in Kela 2 Gas Field, Kuqa Depression, Tarim Basin

doi: 10.3799/dqkx.2016.044
  • Received Date: 2015-09-17
  • Publish Date: 2016-03-15
  • The Kela-2 gas field is the most productive gas field in China. The lower Cretaceous Bashenjiqike Formation (K1bs) are the dominated gas-bearing strata. Characterization of the diagenetic history, different fluid inclusion assemblages and the effects of oil emplacement on diagenetic processes of the K1bs in the Kuqa Depression, Tarim Basin have been studied using a combination of techniques such as polarizing microscope, cathode luminescence (CL), scanning electron microscope (SEM), CT three-dimensional reconstruction, X-ray diffraction (XRD), fluorescence spectroscopy, microthermometry, and Raman microspectroscopy. Diagenetic events identify include quartz overgrowths, early calcite cements, dolomite cements, ankerite cements, micro-quartz and authigenic kaolinite. Three episodes of oil emplacement are recorded by the diagenetic products in the K1bs Formations. The first episode consists of the yellowish-brown fluorescent petroleum inclusions hosted in the transgranular fractures, cleavage plans of the feldspar and calcite cements, paired with low trapped temperature and relatively high salinity, forming around 18 Ma; the second episode consists of the yellow-white to blue-white petroleum inclusions located in the transgranular fractures, boundary of quartz particles and dolomite cements, paired with high trapped temperature and high salinity, forming around 6 Ma; the third episode consists of the CH4-bearing vapour inclusions within the annealed microfractures and ankerite cements, having with high trapped temperature and low salinity, forming around 4 Ma. Authigenic kaolinite, micor-quartz and solid bitumen are the results transformed by the advanced natural gas charge.

     

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