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Information Journal Paper

Title

THERMAL MODELING OF A GACHSARAN CROSS SECTION

Pages

  46-59

Abstract

 Oil generation from source rocks is controlled by time and temperature and formation temperature is affected by various parameters. Thermal history can be reconstructed from burial history whose rate is related to sedimentation rate. Zagros folding has affected source rock properties characteristics. In this study, maturity of Kazdumi and Pabdeh-Gurpi in a cross section through Gachsaran anticline was determined by using THERMAL MODELING. It is shown that maturity and expulsion increased from top anticline toward flanks. KAZDUMI FORMATION entered oil generation from Oligocene to Miocene. The deeper part of Gachsaran anticline Kazdumi is at the end oil window whereas in shallower part it is at the beginning of oil generation. Pabdeh-Gurpi has lower maturity than Kazdumi and only in deep part; it is in early oil generation. Volumetric calculations of Kazdumi oil generation show that the volume of expelled oil varies in different locations. No hydrocarbon was expelled from Pabdeh-Gurpi Fromations.

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    • Cite

    APA: Copy

    ZEYNALZADEH, ARSALAN. (2008). THERMAL MODELING OF A GACHSARAN CROSS SECTION. SHAHID CHAMRAN UNIVERSITY JOURNAL OF SCIENCE, NEW SERIES(19 (SECTION B)), 46-59. SID. https://sid.ir/paper/58033/en

    Vancouver: Copy

    ZEYNALZADEH ARSALAN. THERMAL MODELING OF A GACHSARAN CROSS SECTION. SHAHID CHAMRAN UNIVERSITY JOURNAL OF SCIENCE[Internet]. 2008;NEW SERIES(19 (SECTION B)):46-59. Available from: https://sid.ir/paper/58033/en

    IEEE: Copy

    ARSALAN ZEYNALZADEH, “THERMAL MODELING OF A GACHSARAN CROSS SECTION,” SHAHID CHAMRAN UNIVERSITY JOURNAL OF SCIENCE, vol. NEW SERIES, no. 19 (SECTION B), pp. 46–59, 2008, [Online]. Available: https://sid.ir/paper/58033/en

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