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Information Journal Paper

Title

DIAGENTIC PROCESSES AND GEOCHEMICAL VARIATIONS OF MINOR ELEMENTSAT THE SARVAK FORMATION IN SOUTHERH OF IRAN

Pages

  53-72

Abstract

 The mid Cretaceous (Albia-Truonian) SARVAK FORMATION in the ZAGROS basin of SW Iran is principally composed of carbonates with minor shales and marls. This is the second major oil carbonate reservoir rock in the ZAGROS area. For investigation of effects of DIAGENETIC PROCESSES and trace elements changes on the reservoir properties of this formation are studied 391 thin sections and are analyzed 40 powder samples.The early marine diagenesis is mainly represented by micritization, bioturbation, radiaxial fibrous and syntaxial overgrowth cements, and developed interparticle porosity formations. Meteoric diagenesis includes clean syntaxial and drusy cements, moldic and vuggy porosities formations. Late DIAGENETIC PROCESSES (in shallow and deep burial stages) involve dolomitization, stylolitization, poikilotopic cement, fractures and a little vuggy and moldic porosities formation.The petrographic and elements (Sr, Mn, Na) studies indicate that aragonite was original carbonate mineralogy. Geochemical studies illustrate that these carbonates were affected by meteoric diagenesis in a closed system and trace elements changes prove that with using Sr and Mn values variations can separate facies from each other.

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    APA: Copy

    GHOLAMI ZADEH, P., & ADABI, M.H.. (2011). DIAGENTIC PROCESSES AND GEOCHEMICAL VARIATIONS OF MINOR ELEMENTSAT THE SARVAK FORMATION IN SOUTHERH OF IRAN. JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES, 27(1 (42)), 53-72. SID. https://sid.ir/paper/157113/en

    Vancouver: Copy

    GHOLAMI ZADEH P., ADABI M.H.. DIAGENTIC PROCESSES AND GEOCHEMICAL VARIATIONS OF MINOR ELEMENTSAT THE SARVAK FORMATION IN SOUTHERH OF IRAN. JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES[Internet]. 2011;27(1 (42)):53-72. Available from: https://sid.ir/paper/157113/en

    IEEE: Copy

    P. GHOLAMI ZADEH, and M.H. ADABI, “DIAGENTIC PROCESSES AND GEOCHEMICAL VARIATIONS OF MINOR ELEMENTSAT THE SARVAK FORMATION IN SOUTHERH OF IRAN,” JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES, vol. 27, no. 1 (42), pp. 53–72, 2011, [Online]. Available: https://sid.ir/paper/157113/en

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