SEDIMENTARY ENVIRONMENT, DIAGENESIS AND GEOCHEMISTRY OF CARBONATE ROCKS OF BAHRAM FORMATION (MIDDLE-LATE DEVONIAN) IN QALEH-BALA SECTION (OZBAK-KUH, EAST OF IRAN)

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MAHMOUDI F.; MIRAB SHABESTARI GH.; KHAZAEI A.R.

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Journal: SEDIMENTARY FACIES Year:2015 | Volume:8 | Issue:1 Page(s): 107-130

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Title

SEDIMENTARY ENVIRONMENT, DIAGENESIS AND GEOCHEMISTRY OF CARBONATE ROCKS OF BAHRAM FORMATION (MIDDLE-LATE DEVONIAN) IN QALEH-BALA SECTION (OZBAK-KUH, EAST OF IRAN)

Author(s)

MAHMOUDI F. | MIRAB SHABESTARI GH. | KHAZAEI A.R. | Issue Writer Certificate

Keywords

BAHRAM FORMATIONQ2

OZBAK-KUHQ2

MIDDLE-LATE DEVONIANQ2

CARBONATE RAMPQ2

DIAGENESISQ2

GEOCHEMISTRYQ2

Abstract

Introduction BAHRAM FORMATION (Middle-Late Devonian) is the second stratigraphic unit of the OZBAK-KUH Group in east of Central Iran. It generally consists of bluish-gray to gray limestones which gradually covers dolomites of the Sibzar Formation and is overlaid by Shishtu Formation or with an erosional contact in some regions (Aghanabati, 2010). Most of the previously published works, (e.g. Ahmadi & Ashuri, 1998; Bahariet al., 2006; and Ahmadzadeh Heravi et al., 2007), have had mainly focused on biostratigraphy and lithostratigraphy of BAHRAM FORMATION. But in recent years, some other studies about microfacies, sedimentary environment, sequence stratigraphy and paragenetic sequence of BAHRAM FORMATION have been carried out by Rostamnezhad et al. (2012), Hashemi et al. (2012) and Hoseinabadi et al. (2013). In this research, a stratigraphic section of carbonate rocks of BAHRAM FORMATION with 332 m thickness in the east of OZBAK-KUH village, north of Tabas city (Southern Khorasan Province), has been measured, sampled and studied. This sequence generally has been made of gray colored, thin to thick bedded limestones.

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APA: Copy

MAHMOUDI, F., MIRAB SHABESTARI, GH., & KHAZAEI, A.R.. (2015). SEDIMENTARY ENVIRONMENT, DIAGENESIS AND GEOCHEMISTRY OF CARBONATE ROCKS OF BAHRAM FORMATION (MIDDLE-LATE DEVONIAN) IN QALEH-BALA SECTION (OZBAK-KUH, EAST OF IRAN). SEDIMENTARY FACIES, 8(1), 107-130. SID. https://sid.ir/paper/199820/en

Vancouver: Copy

MAHMOUDI F., MIRAB SHABESTARI GH., KHAZAEI A.R.. SEDIMENTARY ENVIRONMENT, DIAGENESIS AND GEOCHEMISTRY OF CARBONATE ROCKS OF BAHRAM FORMATION (MIDDLE-LATE DEVONIAN) IN QALEH-BALA SECTION (OZBAK-KUH, EAST OF IRAN). SEDIMENTARY FACIES[Internet]. 2015;8(1):107-130. Available from: https://sid.ir/paper/199820/en

IEEE: Copy

F. MAHMOUDI, GH. MIRAB SHABESTARI, and A.R. KHAZAEI, “SEDIMENTARY ENVIRONMENT, DIAGENESIS AND GEOCHEMISTRY OF CARBONATE ROCKS OF BAHRAM FORMATION (MIDDLE-LATE DEVONIAN) IN QALEH-BALA SECTION (OZBAK-KUH, EAST OF IRAN),” SEDIMENTARY FACIES, vol. 8, no. 1, pp. 107–130, 2015, [Online]. Available: https://sid.ir/paper/199820/en

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