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LI Hui li, QIU Nan sheng, JIN Zhi jun, LU Xiu xiang. Study on Hydrocarbon Entrapment in Kela 2 Gas Field,Tarim Basin[J]. Acta Sedimentologica Sinica, 2003, 21(4): 648-653.
Citation: LI Hui li, QIU Nan sheng, JIN Zhi jun, LU Xiu xiang. Study on Hydrocarbon Entrapment in Kela 2 Gas Field,Tarim Basin[J]. Acta Sedimentologica Sinica, 2003, 21(4): 648-653.

Study on Hydrocarbon Entrapment in Kela 2 Gas Field,Tarim Basin

  • Received Date: 2002-10-17
  • Rev Recd Date: 2003-01-21
  • Publish Date: 2003-12-10
  • The analysis of reservoir fluid inclusions is a useful method in studying hydrocarbon migration and entrapment.Four homogenization temperature groups, 75 ~ 105 ℃, 120 ~ 135 ℃, 155 ~ 175 ℃ and 200 ~ 250 ℃, are obtained, based on testing reservoir fluid inclusions systematically sampled from Well Kela-201 in Kela 2 gas field. The former three homogenization temperature groups are related to the hydrocarbon entrapment in Kela 2 gas field, and the last one or the higher temperatures may be related to the action of the hydrothermal fluid from the deep.In combination with the reconst ruction of the burial history and thermal history, it is shown that the time of hydrocarbon entrapment in Kela 2 gas field is 11 ~ 2.5Ma, beginning at the sedimentary time of Kangcun Formation to Kuche Formation and ending at the denudation time of Kuche Formation.The gas field could be altered by the action of hydrothermal fluid.
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  • Received:  2002-10-17
  • Revised:  2003-01-21
  • Published:  2003-12-10

Study on Hydrocarbon Entrapment in Kela 2 Gas Field,Tarim Basin

Abstract: The analysis of reservoir fluid inclusions is a useful method in studying hydrocarbon migration and entrapment.Four homogenization temperature groups, 75 ~ 105 ℃, 120 ~ 135 ℃, 155 ~ 175 ℃ and 200 ~ 250 ℃, are obtained, based on testing reservoir fluid inclusions systematically sampled from Well Kela-201 in Kela 2 gas field. The former three homogenization temperature groups are related to the hydrocarbon entrapment in Kela 2 gas field, and the last one or the higher temperatures may be related to the action of the hydrothermal fluid from the deep.In combination with the reconst ruction of the burial history and thermal history, it is shown that the time of hydrocarbon entrapment in Kela 2 gas field is 11 ~ 2.5Ma, beginning at the sedimentary time of Kangcun Formation to Kuche Formation and ending at the denudation time of Kuche Formation.The gas field could be altered by the action of hydrothermal fluid.

LI Hui li, QIU Nan sheng, JIN Zhi jun, LU Xiu xiang. Study on Hydrocarbon Entrapment in Kela 2 Gas Field,Tarim Basin[J]. Acta Sedimentologica Sinica, 2003, 21(4): 648-653.
Citation: LI Hui li, QIU Nan sheng, JIN Zhi jun, LU Xiu xiang. Study on Hydrocarbon Entrapment in Kela 2 Gas Field,Tarim Basin[J]. Acta Sedimentologica Sinica, 2003, 21(4): 648-653.
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