ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
藏北羌塘盆地胜利河油页岩干酪根特征及碳同位素指示意义
  
关键词:Qiangtang basin  Shengli River oil shale  kerogen  carbon isotope
基金项目:国家自然科学基金项目(编号: 40702020)、四川省青年科技基金(09ZQ026-006)和国家油气专项(编号: XQ2004-06)资助
作者单位E-mail
付修根 成都地质矿产研究所, 四川成都 610081 fuxiugn@126.com 
王剑 成都地质矿产研究所, 四川成都 610081  
汪正江 成都地质矿产研究所, 四川成都 610081  
何江林 成都地质矿产研究所, 四川成都 610081  
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摘要:
Characteristics of Kerogens and Their Carbon Isotope Implications for the Shengli River Oil Shale in Qiangtang Basin, Northern Tibet
      The Shengli River oil shale in the southern part of northern Qiangtang depression within northern Tibet plateau has a EW-extending length of more than 34 km and a width of 9 m in the north-south direction. Such oil shale is of great importance in the assessment of oil and gas resources in Qiangtang basin. The oil shale has high kerogen contents and H/C ratios (1.11~1.19) and low O/C values (0.08~0.25), implying a fairly ideal source rock. The oil shale and interbedded marl from the Shengli River area in Qiangtang basin have a remarkably heavy Ckerogen isotopic composition, ranging in δ13C values of the bulk organic matter from -20.79‰ to -21.78‰. The enrichment of 13C in the Shengli River oil shale can be attributed to a combination of the high growth rate and the sedimentary environment, with the paleo-lagoon environment obviously controlling the spatial distribution and size of oil shale.
FU Xiu-gen,WANG Jian,WANG Zheng-jiang,HE Jiang-lin.2009.Characteristics of Kerogens and Their Carbon Isotope Implications for the Shengli River Oil Shale in Qiangtang Basin, Northern Tibet[J].Acta Geoscientica Sinica,30(5):643-650.
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