Articles

Petrology characteristics and the origin of dawsonite-bearing sandstone reservoir in southern Songliao Basin

  • QU Xiyu ,
  • ZHU Wenhui ,
  • LIU Li ,
  • DONG Fuxiang
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  • 1. School of Geosciences, China University of Petroleum, Qingdao 266580, China;
    2. College of Earth Science, Jilin University, Changchun 130061, China;
    3. Changchun Institute of Technology, Changchun 130021, China

Received date: 2014-12-24

  Revised date: 2015-01-16

  Online published: 2015-05-04

Abstract

This paper studies the petrologic characteristics of the dawsonite- bearing sandstone reservoirs of the Cretaceous in southern Songliao Basin,the diagenetic sequence of the dawsonite-bearing sandstone, and the occurrence and the origin of the dawsonite based on the principles and the methods of the petrology and the isotope geochemistry. The petrologic study shows that the dawsonite-bearing sandstones are mainly composed of the arkoses and the feldspathic litharenite. The diagenetic sequence is shown to be the clay coating cementation-secondary feldspar overgrowth-secondary quartz overgrowth, authigenic quartz, kaolinite-calcitehydrocarbon charging-CO2 charging-dawsonite-ankerite. The analysis of the carbon and oxygen isotope composition indicates that the dawsonite δ13CPDB values range from -0.342% to 0.329%, and δ18OPDB values range from -1.922% to -0.954%, as is similar to the proved dawsonite formed in the organic background and related to the magmatic activity. The calculated δ13CPDB values of CO2 gas in the isotope equilibrium with the dawsonite ranging from -0.992% to -0.423%, are consistent with the δ13CPDB values of the inorganic CO2 in the southern Songliao Basin. These values indicate that the CO2 that forms the dawsonite and that from the gas reservoir have the same source, which is the mantle-sourced origin.

Cite this article

QU Xiyu , ZHU Wenhui , LIU Li , DONG Fuxiang . Petrology characteristics and the origin of dawsonite-bearing sandstone reservoir in southern Songliao Basin[J]. Science & Technology Review, 2015 , 33(7) : 13 -19 . DOI: 10.3981/j.issn.1000-7857.2015.07.001

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