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The characteristics of unconformity surface at the bottom of the Paleogene and its significance in hydrocarbon migration in the Sikeshu Sag of the Junggar Basin, Northwest China 被引量:2

The characteristics of unconformity surface at the bottom of the Paleogene and its significance in hydrocarbon migration in the Sikeshu Sag of the Junggar Basin, Northwest China
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摘要 The unconformity surface at the bottom of the Paleogene, located in the Sikeshu Sag of the Junggar Basin, Northwest China, is one of the most important hydrocarbon migration pathways and characterized by 3 layers of upper coarse clastic rock, lower weathering crust and leached zone. The upper coarse clastic rock displays features of higher density, lower SDT and gamma-ray logging while the weathering crust in the lower part displays opposite features. The formation water is of NaHCO 3 type but at lower mineralization degree. The QGF indices are generally between 2.19 and 3.77 and the GOI parameters vary from 1% to 5%. From the southeast to the northwest of the sag, the content of saturated hydrocarbon increases from 30.81% to 53.74% while that of non-hydrocarbon and asphaltene decreases. The Pr/nC 17 decreases from 0.65 to 0.47 while the Ph/nC 18 decreases from 0.66 to 0.27, and the content of benzo[c] carbazole declines while the benzo[a] carbazole amount and (alkyl carbazole)/(alkyl+benzo carbazole) ratio both increase. These revealed that the hydrocarbons migrated from the sag to the ramp region along the unconformity surface. The unconformity surface at the bottom of the Paleogene, located in the Sikeshu Sag of the Junggar Ba- sin, Northwest China, is one of the most important hydrocarbon migration pathways and characterized by 3 layers of upper coarse clastic rock, lower weathering crust and leached zone. The upper coarse elastic rock displays features of higher density, lower SDT and gamma-ray logging while the weathering crust in the lower part displays opposite features. The formation water is of NaHCO3 type but at lower mineralization degree. The QGF indices are generally between 2.19 and 3.77 and the GOI parameters vary from 1% to 5%. From the southeast to the northwest of the sag, the content of saturated hydrocarbon increases from 30.81% to 53.74% while that of non-hydrocarbon and asphaltene decreases. The Pr/nC17 decreases from 0.65 to 0.47 while the Ph/nC18 decreases from 0.66 to 0.27, and the content of benzo[c] carbazole declines while the benzo[a] carbazole amount and (alkyl carbazole)/(alkyl+benzo carba- zole) ratio both increase. These revealed that the hydrocarbons migrated from the sag to the ramp region along the unconformity surface.
出处 《Chinese Journal Of Geochemistry》 EI CAS CSCD 2013年第2期181-190,共10页 中国地球化学学报
基金 financially supported jointly by the National Key Project of Science and Technology for Development of Large-size Oil & gas Fields and Coal-bed Gas (Grant No. 2008ZX05003-002) the State Key Laboratory of Petroleum Resources and Prospecting (No. prp2009-02)
关键词 中国西北地区 油气运移通道 准噶尔盆地 不整合面 古近系 凹陷 底部 苯并咔唑 hydrocarbon migration and accumulation unconformity surface Paleogene Sikeshu Sag Junggar Basin
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