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Information Journal Paper

Title

RECONSTRUCTION OF SEDIMENTARY ENVIRONMENT OF FARAGHAN FORMATION IN DARANG #1 WELL

Pages

  89-97

Abstract

 In this study, depositional environment of the FARAGHAN FORMATION has been interpreted in DARANG #1 well. Petrography studies of the cuttings led to identification of five petrofacies that according to their abundance include: lithic arenite, quartz arenite, greywacke, hybrid arenite and mudstone. More than 90 percent of this succession is composed of lithic arenites with volcanic rock fragments and fine grained quartz arenite. In this study, we combined PETROFACIES ANALYSIS and gamma ray logs to reconstruct SEDIMENTARY ENVIRONMENT of this formation. According to our data, six SEDIMENTARY FACIES has been identified. Therefore the FARAGHAN FORMATION has been deposited in the upstream parts of delta plain to delta front in the lower part and shallow marine in the upper part of the succession which grades upward into a carbonate shelf deposit of Dalan Formation.

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    APA: Copy

    ZAMANZADEH, S.M., MIRZAEE, S., SARDAR, H., & SHEGEFT FARD, M.. (2010). RECONSTRUCTION OF SEDIMENTARY ENVIRONMENT OF FARAGHAN FORMATION IN DARANG #1 WELL. IRANIAN JOURNAL OF GEOLOGY, 4(13), 89-97. SID. https://sid.ir/paper/129299/en

    Vancouver: Copy

    ZAMANZADEH S.M., MIRZAEE S., SARDAR H., SHEGEFT FARD M.. RECONSTRUCTION OF SEDIMENTARY ENVIRONMENT OF FARAGHAN FORMATION IN DARANG #1 WELL. IRANIAN JOURNAL OF GEOLOGY[Internet]. 2010;4(13):89-97. Available from: https://sid.ir/paper/129299/en

    IEEE: Copy

    S.M. ZAMANZADEH, S. MIRZAEE, H. SARDAR, and M. SHEGEFT FARD, “RECONSTRUCTION OF SEDIMENTARY ENVIRONMENT OF FARAGHAN FORMATION IN DARANG #1 WELL,” IRANIAN JOURNAL OF GEOLOGY, vol. 4, no. 13, pp. 89–97, 2010, [Online]. Available: https://sid.ir/paper/129299/en

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