EVALUATION OF HYDROCARBON POTENTIAL OF SOURCE ROCKS IN MARUN OILFIELD USING ROCK-EVAL 6

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ALIZADEH BAHRAM; ADAABI M.H.; TEZHEH F.

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Journal: JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT) Year:2006 | Volume:32 | Issue:3 (SECTION GEOLOGY 2) Page(s): 267-274

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Title

EVALUATION OF HYDROCARBON POTENTIAL OF SOURCE ROCKS IN MARUN OILFIELD USING ROCK-EVAL 6

Author(s)

ALIZADEH BAHRAM | ADAABI M.H. | TEZHEH F. | Issue Writer Certificate

Keywords

MARUN OILFIELDQ3

SOURCE ROCKQ3

ROCK- EVAL6Q3

OIL WINDOWQ3

KEROGENQ3

Abstract

Genetic potential of four probable SOURCE ROCKs in MARUN OILFIELD; Pabdeh, Gurpi, Kazhdumi and Garau were investigated. It shows that only pabdeh and particularly Kazhdumi Formations have potent ial to generate hydrocarbons. The Hydrogen Index (HI) vs. Total Organic Carbon (TOC) in four formations indicates direct relation between the two parameters. Kazhdumi Formation with high Hydrogen Index comprises higher amount of total organic carbon. This could be due to reducing environment of organic matter depositional conditions. Maximum Temperature (Tmax) and depth variations shown by diagram in well No. 123 and 222 of Bangestan reservoir in MARUN OILFIELD indicate that inbothwells Sarvak shales are just at the beginning of OIL WINDOW, but in well No. 222 Tmax variation versus depth is more severe and Tmax is higher in Kazhdumi Formations. Plot of S2 vs. TOC for inert carbon determination indicates 0.5% in Pabdeh and Gurpi, whereas inert carbons in Kazhdumi are not more than 0.25%. Organic facies curves for Kazhdumi and Garau places them in B to BC zones showing marine reducing with minor oxidizing environment. In Pabdeh and Gurpi, organic facies is variable and consist of a mixture of marine and terrestrial organic matter, indicating transgression and regression of the sea. The van Krevelen diagram indicates KEROGEN type II/III for all formations, but only Kazhdumi Formation is in the cat agenesis and OIL WINDOW territory. Finally, among the four studied formations, Kazhdumi with highest organic carbon and optimum thermal maturation is introduced as the best SOURCE ROCK for MARUN OILFIELD.

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APA: Copy

ALIZADEH, BAHRAM, ADAABI, M.H., & TEZHEH, F.. (2006). EVALUATION OF HYDROCARBON POTENTIAL OF SOURCE ROCKS IN MARUN OILFIELD USING ROCK-EVAL 6. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), 32(3 (SECTION GEOLOGY 2)), 267-274. SID. https://sid.ir/paper/2301/en

Vancouver: Copy

ALIZADEH BAHRAM, ADAABI M.H., TEZHEH F.. EVALUATION OF HYDROCARBON POTENTIAL OF SOURCE ROCKS IN MARUN OILFIELD USING ROCK-EVAL 6. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT)[Internet]. 2006;32(3 (SECTION GEOLOGY 2)):267-274. Available from: https://sid.ir/paper/2301/en

IEEE: Copy

BAHRAM ALIZADEH, M.H. ADAABI, and F. TEZHEH, “EVALUATION OF HYDROCARBON POTENTIAL OF SOURCE ROCKS IN MARUN OILFIELD USING ROCK-EVAL 6,” JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), vol. 32, no. 3 (SECTION GEOLOGY 2), pp. 267–274, 2006, [Online]. Available: https://sid.ir/paper/2301/en

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