MICROFACIES ANALYSIS AND DEPOSITIONAL ENVIRONMENTS OF THE ASMARI FORMATION AT THE GHAR-E AGHA SEYYED SECTION, FARSAN AREA (CHAHARMAHAL BAKHTIARI PROVINCE), HIGH ZAGROS

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HAMIDZADEH S.M.; BABAZADEH S.A.; ASGARI PIRBALUTI B.; SOLGI A.

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Journal: GEOSCIENCES Year:2017 | Volume:27 | Issue:105 Page(s): 25-32

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Title

MICROFACIES ANALYSIS AND DEPOSITIONAL ENVIRONMENTS OF THE ASMARI FORMATION AT THE GHAR-E AGHA SEYYED SECTION, FARSAN AREA (CHAHARMAHAL BAKHTIARI PROVINCE), HIGH ZAGROS

Author(s)

HAMIDZADEH S.M. | BABAZADEH S.A. | ASGARI PIRBALUTI B. | SOLGI A. | Issue Writer Certificate

Keywords

ASMARI FORMATIONQ2

MICROFACIESQ2

FARSANQ1

GHAR-E AGHA SEYYEDQ1

Abstract

The ASMARI FORMATION was measured and sampled at GHAR-E AGHA SEYYED in FARSAN area in order to determine sedimentary environment based on facies analysis. In the study area, the ASMARI FORMATION has a thickness of 183 m and conformably overlain the Pabdeh Formation. Based on MICROFACIES studies, eight MICROFACIES were recognized including: 1) Porcelanouse foraminifera – bioclastic – red algal wackestone / packstone, 2) Rotalia grainstone, 3) Bioclastic –red algal grainstone, 4) Red algal – coral boundstone, 5) Red algal wackestone (Floatstone), 6) Red algal –large hyaline foraminifera – intraclast packstone, 7) Red algal – bioclastic - large hyaline foraminifera wackestone / packstone, 8) Large hyaline foraminifera packstone. These MICROFACIES represent three facies belts including Inner ramp, Middle ramp and Outer ramp. Based on the presence of benthic foraminifera, age of Oligocene (Rupelian – Chatian) is determined for the Asmari Fm. at this section.

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APA: Copy

HAMIDZADEH, S.M., BABAZADEH, S.A., ASGARI PIRBALUTI, B., & SOLGI, A.. (2017). MICROFACIES ANALYSIS AND DEPOSITIONAL ENVIRONMENTS OF THE ASMARI FORMATION AT THE GHAR-E AGHA SEYYED SECTION, FARSAN AREA (CHAHARMAHAL BAKHTIARI PROVINCE), HIGH ZAGROS. GEOSCIENCES, 27(105 ), 25-32. SID. https://sid.ir/paper/32258/en

Vancouver: Copy

HAMIDZADEH S.M., BABAZADEH S.A., ASGARI PIRBALUTI B., SOLGI A.. MICROFACIES ANALYSIS AND DEPOSITIONAL ENVIRONMENTS OF THE ASMARI FORMATION AT THE GHAR-E AGHA SEYYED SECTION, FARSAN AREA (CHAHARMAHAL BAKHTIARI PROVINCE), HIGH ZAGROS. GEOSCIENCES[Internet]. 2017;27(105 ):25-32. Available from: https://sid.ir/paper/32258/en

IEEE: Copy

S.M. HAMIDZADEH, S.A. BABAZADEH, B. ASGARI PIRBALUTI, and A. SOLGI, “MICROFACIES ANALYSIS AND DEPOSITIONAL ENVIRONMENTS OF THE ASMARI FORMATION AT THE GHAR-E AGHA SEYYED SECTION, FARSAN AREA (CHAHARMAHAL BAKHTIARI PROVINCE), HIGH ZAGROS,” GEOSCIENCES, vol. 27, no. 105 , pp. 25–32, 2017, [Online]. Available: https://sid.ir/paper/32258/en

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