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Information Journal Paper

Title

INVESTIGATING SOURCE ROCK ZONES IN THE DARKHOVAIN OIL FIELD BY USING PETROPHYSICS AND ROCK EVAL ANALYSIS

Pages

  63-70

Abstract

 Source rock is one of main elements in petroelum system. In order to investigate a petroleum system in an oil region, it's necessary to recognize the characteristics of source rocks. In this study the source rocks of the Darkhovain oil field in Abadan plan are investigated. In this way, gamma rays and SONIC LOG are used and SOURCE ROCK ZONES separated in Pabdeh, Garu, Gotnia, Najmeh, Sargelu and Nyriz formations. These zones sampled and total organic carbon of samples determined with ROCK EVAL ANALYSIS. Acording to Rock Eval results, Sargelu and Garu zones have good to excellent total organic carbon and good to moderate genetic potential. These zones have more thickness then the other zones. Kazdumi source rock samples show range of good to very good in total organic carbon and a range of moderate to good in genetic potential. Pabdeh, Sarvak and Surgah samples are poor in organic matter and have low genetic potential. Acording to this study, Sargrlu and Garu zones are main source rocks and Kazdumi and Nyriz zones are minor source rocks in DARKHOVAIN FIELD.

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    APA: Copy

    ZEINALZADEH, A., & SAJADIAN, V.A.. (2009). INVESTIGATING SOURCE ROCK ZONES IN THE DARKHOVAIN OIL FIELD BY USING PETROPHYSICS AND ROCK EVAL ANALYSIS. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), 35(3 (SECTION: GEOLOGY)), 63-70. SID. https://sid.ir/paper/2255/en

    Vancouver: Copy

    ZEINALZADEH A., SAJADIAN V.A.. INVESTIGATING SOURCE ROCK ZONES IN THE DARKHOVAIN OIL FIELD BY USING PETROPHYSICS AND ROCK EVAL ANALYSIS. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT)[Internet]. 2009;35(3 (SECTION: GEOLOGY)):63-70. Available from: https://sid.ir/paper/2255/en

    IEEE: Copy

    A. ZEINALZADEH, and V.A. SAJADIAN, “INVESTIGATING SOURCE ROCK ZONES IN THE DARKHOVAIN OIL FIELD BY USING PETROPHYSICS AND ROCK EVAL ANALYSIS,” JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), vol. 35, no. 3 (SECTION: GEOLOGY), pp. 63–70, 2009, [Online]. Available: https://sid.ir/paper/2255/en

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