西南石油大学学报(自然科学版) ›› 2007, Vol. 29 ›› Issue (5): 34-37.DOI: 10.3863/j.issn.1000-2634.2007.05.09

• 地质勘探 • Previous Articles     Next Articles

GAS COMPONENTS AND THE ORIGIN IN FEIXIANGUAN FORMATION GAS POOL, NORTHEAST OF SICHUAN

ZHU Ya-dong1,2 WANG Yun-cheng1 GAO Pei-cheng2 et al.   

  1. College of Energy Resources,Chengdu University of Technology,Chengdu Sichuan 610054,China
  • Received:2007-01-20 Revised:1900-01-01 Online:2007-10-20 Published:2007-10-20
  • Contact: ZHU Ya-dong

Abstract: In northeast Sichuan Basin, Feixianguan Formation gas pools are rupewrdry gas ones with lots of H2S, over matured, and the pressure are normal or lower. The strata were embeded deeply and experienced high temperature in geologic history, the conditions that oil cracked into gas existed. The components of fluid inclusions prove the original Feixianguan Formation gas pool contains a lot C+2 hydrocarbons and liquid bitumen, but no H2S, and prove that the gas pool evolved from crude oil. The there was thermochemical reduction reaction between cracked gas and sulphate, consumed a lot C+2 hydrocarbons,generated lots of H2S and CO2. So,the gas pool contain lots of H2S,and has over matured character. TSR generated a lot acid, the acid eroded the reservoir and increased the pore space. Furthermore, a great lot of H2S and CO2 dissolved in water,so, the pressure of gas pool is lower.

Key words: Feixianguan Formation, cracking gas, thermochemical sulphate reduction(TSR), fluid inclusion, Sichuan Basin

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