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柴达木盆地三湖地区北斜坡岩性地层气藏形成的地质条件与预测技术研究

The lithologic and stratigraphic gas reservoirs in the north slope of the sanhu area,Qaidam basin:a study on their genetic conditions and characterization techniques

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【作者】 苏明军王西文何亨华刘彩燕袁克峰

【Author】 SU Ming-jun1,2,WANG Xi-wen2,HE Heng-hua 2,LIU Cai-yan2,Yuan Ke-feng3(1.China University of Petroleum,Beijing 102249,China;2.Northwest Subsidiary of PetroChina Researchh Institute of Petroleum Exploration & Development,Gansu 730020,China;3.CNPC International Research Center,Beijing 100083)

【机构】 中国石油大学中国石油勘探开发研究院西北分院中油国际海外研究中心

【摘要】 三湖地区北斜坡褶皱发育,相变快,生储盖组合优越,具备形成岩性地层气藏的构造背景和地质条件.由于本区储层厚度薄(1~3m),缺乏三维地震资料,砂体分布难以准确追踪,导致岩性地层气藏勘探难以取得突破.已知气藏解剖和理论研究表明地层含气后会产生特殊的地震响应,通过地震异常信息研究,结合构造、沉积和成藏条件分析,发现驼西地区是岩性圈闭发育带,Tzh2井获得工业气流证明该区带具备形成岩性气区的潜力.

【Abstract】 The north slope of the Sanhu area of the Qaidam basin,with its characteristic geologic features such as strong fold,rapid lithofacies variation,promising geologic setting,is prone to have stratigraphic and lithologic gas pools.However,as the reservoir beds are extremely thin(1~3 meters),and lack of 3D seismic data,it is very difficult to identify the sand bodies and trace them laterally,resulting in a very low discovery rate of stratigraphic-lithologic reservoirs.Studies on producing gas trap and theoretical reasoning indicate that abnormal seismic response will be observed when the reservoir is gas accumulated.As a result,based on abnormal seismic response analysis,accompanied by studies on structural,sedimentary,and accumulation conditions,the Tuoxi belt was recognized as a lithologic trap region.A well,Tzh2,drilled afterwards in this belt,showed commercial gas,indicating promising potential of lithologic gas pool in this region.

【基金】 中国石油天然气股份公司科技攻关项目(050110-3)资助
  • 【文献出处】 地球物理学进展 ,Progress in Geophysics , 编辑部邮箱 ,2008年04期
  • 【分类号】P618.13
  • 【被引频次】9
  • 【下载频次】185
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