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Article Navigation >  Acta Sedimentologica Sinica  > 2008  >  26(4): 683-687

YUAN Wen-fang. Characteristic of Dinosterane and C31 Sterane in Paleocene Saline  Formation of Jiyang Depression[J]. Acta Sedimentologica Sinica, 2008, 26(4): 683-687.
Citation: YUAN Wen-fang. Characteristic of Dinosterane and C31 Sterane in Paleocene Saline  Formation of Jiyang Depression[J]. Acta Sedimentologica Sinica, 2008, 26(4): 683-687.
shu

Characteristic of Dinosterane and C31 Sterane in Paleocene Saline  Formation of Jiyang Depression

  • Institute of Exploration and Development , PetroChina Tarim Oil field Company , Kuerle Xinjiang 84100

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  • Corresponding author: YUAN Wen-fang
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2008-08-10
  • The study on chromatography mass analysis of saturated hydrocarbons in Paleogene saline formation of Jiyang Depression shows that dinosterane and C31sterane developed in source rocks of the 1st member（Es1）, the 3rd member（Es3）and upper the 4th member（EsU4）of Shahejie Formation, these molecular fossils are marks of marine transgression, moreover C31sterane denotes that the formation is influenced more by sea water, therefore salinity of 3 members related to marine transgression.
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  • Received:  1900-01-01
  • Revised:  1900-01-01
  • Published:  2008-08-10

Characteristic of Dinosterane and C31 Sterane in Paleocene Saline  Formation of Jiyang Depression

  • Institute of Exploration and Development , PetroChina Tarim Oil field Company , Kuerle Xinjiang 84100
    Corresponding author: YUAN Wen-fang
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2008-08-10

Abstract: The study on chromatography mass analysis of saturated hydrocarbons in Paleogene saline formation of Jiyang Depression shows that dinosterane and C31sterane developed in source rocks of the 1st member（Es1）, the 3rd member（Es3）and upper the 4th member（EsU4）of Shahejie Formation, these molecular fossils are marks of marine transgression, moreover C31sterane denotes that the formation is influenced more by sea water, therefore salinity of 3 members related to marine transgression.

YUAN Wen-fang. Characteristic of Dinosterane and C31 Sterane in Paleocene Saline  Formation of Jiyang Depression[J]. Acta Sedimentologica Sinica, 2008, 26(4): 683-687.
Citation: YUAN Wen-fang. Characteristic of Dinosterane and C31 Sterane in Paleocene Saline  Formation of Jiyang Depression[J]. Acta Sedimentologica Sinica, 2008, 26(4): 683-687.
shu

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