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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2003  >  25(6): 769-772
WANG Shi-hu, LI Zheng, XIA Bin, CHEN Gen-wen, YAN Yi, YU Jun-feng, CHEN Zhi-yong. CHARACTERISTICS OF HYDROCARBON SOURCE ROCKS IN THEJURASSIC SHEMSHAK FORMATION OF KASHAN AREA, IRAN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2003, 25(6): 769-772. doi: 10.11781/sysydz200306769
Citation: WANG Shi-hu, LI Zheng, XIA Bin, CHEN Gen-wen, YAN Yi, YU Jun-feng, CHEN Zhi-yong. CHARACTERISTICS OF HYDROCARBON SOURCE ROCKS IN THEJURASSIC SHEMSHAK FORMATION OF KASHAN AREA, IRAN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2003, 25(6): 769-772. doi: 10.11781/sysydz200306769
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CHARACTERISTICS OF HYDROCARBON SOURCE ROCKS IN THEJURASSIC SHEMSHAK FORMATION OF KASHAN AREA, IRAN

doi: 10.11781/sysydz200306769
  • 1.

    Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, Guangdong 510640, China

  • 2. Shengli Oilfield, Dongying, Shangdong 257001, China

  • Received Date: 2003-05-28
  • Rev Recd Date: 2003-10-11
  • Publish Date: 2003-11-25
    Abstract
  • By analyses on the organic matter abundance of hydrocarbon source rocks,the vitrinite composition and carbon isotopic features of kerogen and the features of biomarkers in the Jurassic Shemshak Formation of Kashan area,Iran,it was suggested that the kerogen types of the Shemshak source rocks be mainly sapropel-humic(Ⅱ2) and humic(Ⅲ).Most samples have evolved to overmature stages.Except for a few good source rocks,most source rocks of the Shemshak Formation are middle grade.

     

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    • References(3)
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    程克明,王兆云,钟宁宁,等.碳酸盐油气成藏理论与实践[M].北京:石油工业出版社,1996.29-90.
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    郝石生,高岗,刚文哲,等.高过成熟海相碳酸盐岩[M].北京:石油工业出版社,1996.101-108.
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