Characteristics and Origin of Crude Oils from Well Tazhong 82 Area of Tazhong Uplift

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  • 1. Research Institute of Petroleum Exploration and Develpment,PetroChina, Beijing 100083, China; 2. State Key laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China; 3. Langfang Branch of Research Institute of Petroleum Exploration and Development, CNPC, Langfang 065007, China

Received date: 2007-11-26

  Revised date: 2008-10-09

  Online published: 2008-12-10

Abstract

This paper discussed the characteristics and origin of crude oils found in well Tazhong 82 area by systematic geochemical analysis. It shows that saturate fraction is the main component in the oils, while low carbon nalkanes are the main composition of the saturated hydrocarbon, the ratio of C21-/C 22+ranging from 1.4 to 5.4 and the biomarker content being very low. After n-alkanes being removed by molecule sieves, the biomarker content is still very low, the sterane contents of C27-C28-C29 have the distribution of “V” style, and the contents of rearranged steranes are high; the contents of tricyclic terpanes are higher and pentacyclic terpanes are very low in terpanes, C20 or C23 is predominant in tricyclic terpanes. Triaromatic sterances can not be clearly distinguished; dibenzothiophene present in a higher content, and δ13C ratio is light with a saturate δ13C ratio less than -32.8‰. These characteristics are different from Cambrian oils of well Tadong 2. MPI index shows that maturity of oils is about 0.8% (RO), which indicates that the oils of well Tazhong 82 area are not the products generated by organic matter at higher maturity, but were generatedy Ordovician organic matter with moderate maturity, and were flooded by Cambrian natural gas after accumulation, and accumulated again in the present reservoir.

Cite this article

GUO Jian-jun ;CHEN Jian-fa ;WANG Yi-feng ; SHI Sheng-bao ;MIAO Zhong-ying . Characteristics and Origin of Crude Oils from Well Tazhong 82 Area of Tazhong Uplift[J]. Natural Gas Geoscience, 2008 , 19(06) : 770 -774 . DOI: 10.11764/j.issn.1672-1926.2008.06.770

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