MICROFACIES AND SEDIMENTARY ENVIRONMENT OF THE ILAM FORMATION IN SEMIROM

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MOGHADDAM H.V.; SAFARI ATEFEH

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Paper Information

Journal: RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE" Year:2001 | Volume:15 | Issue:1-2 Page(s): 79-92

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Title

MICROFACIES AND SEDIMENTARY ENVIRONMENT OF THE ILAM FORMATION IN SEMIROM

Author(s)

MOGHADDAM H.V. | SAFARI ATEFEH | Issue Writer Certificate

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Abstract

In order to determine the microfacies and sedimentary environment of the Ilam formation, one stratigraphic column in SW of Semirom (Landaran Anticline) was sampled and studied. Sediments of the Ham formation in the area are dominantly of limestone and marly limestones. Study of petrography indicates that carbonate sediments of the Ilam formation can be divided into 8 groups of carbonate microfacies. Microscopic studies and field obserbations show that the carbonate microfacies form in four sub - sedimentary environments, including: Open marine, Barrier, Lagoon and Tidal Flat. The absence of build-up, slump and turbbidite currents indicate that the carbonate platform of the Ilam formation is a homoclinal ramp. presence of rudist debries indicates a protozoan assemblage and suggests a tropical condition for deposition of the carbonate sediments.

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بررسی میکروفاسیسها و محیط رسوبی سازند سروک در مناطق خوزستان و لرستان

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APA: Copy

MOGHADDAM, H.V., & SAFARI, ATEFEH. (2001). MICROFACIES AND SEDIMENTARY ENVIRONMENT OF THE ILAM FORMATION IN SEMIROM . RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", 15(1-2), 79-92. SID. https://sid.ir/paper/55879/en

Vancouver: Copy

MOGHADDAM H.V., SAFARI ATEFEH. MICROFACIES AND SEDIMENTARY ENVIRONMENT OF THE ILAM FORMATION IN SEMIROM . RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE"[Internet]. 2001;15(1-2):79-92. Available from: https://sid.ir/paper/55879/en

IEEE: Copy

H.V. MOGHADDAM, and ATEFEH SAFARI, “MICROFACIES AND SEDIMENTARY ENVIRONMENT OF THE ILAM FORMATION IN SEMIROM ,” RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", vol. 15, no. 1-2, pp. 79–92, 2001, [Online]. Available: https://sid.ir/paper/55879/en

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