PETROGRAPHY ,ORIGINAL CORBONAT MINERALOGY, AND RECONSTRUCTION OF SEDIMENTARY

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ADAABI M.H.; ARBAB B.

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Journal: JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY) Year:2003 | Volume:2 | Issue:3-4 Page(s): 63-87

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Title

PETROGRAPHY ,ORIGINAL CORBONAT MINERALOGY, AND RECONSTRUCTION OF SEDIMENTARY

Author(s)

ADAABI M.H. | ARBAB B. | Issue Writer Certificate

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Abstract

Mobarak Formation consisting of thick carbonate successions was formed ring Lower Carboniferous in Am area, Central Alborz, near Tehran. This Formation due to disconformably overlain by Dorud (Lower Permian) and underlain by Geirud Formation. Major and minor elements and behavior of δl8O and δl3 C values with trace elements are used for recognition of original carbonate mineralogy. These carbonates are affected mostly by eteoric diagnosis. Facies analysis and petrographic studies led to recognition of 14 microfacies deposited in an-open marine, barrier, lagoon and tidal flat environments. The high Sr concentration is due to aragonitic components deposited in lagoon and back barrier settings. Barrier and open marine facies have low Sr and high Fe, Mn and Na concentrations. A ramp platform is suggested as a depositional environment.

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APA: Copy

ADAABI, M.H., & ARBAB, B.. (2003). PETROGRAPHY ,ORIGINAL CORBONAT MINERALOGY, AND RECONSTRUCTION OF SEDIMENTARY. JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY), 2(3-4), 63-87. SID. https://sid.ir/paper/44095/en

Vancouver: Copy

ADAABI M.H., ARBAB B.. PETROGRAPHY ,ORIGINAL CORBONAT MINERALOGY, AND RECONSTRUCTION OF SEDIMENTARY. JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY)[Internet]. 2003;2(3-4):63-87. Available from: https://sid.ir/paper/44095/en

IEEE: Copy

M.H. ADAABI, and B. ARBAB, “PETROGRAPHY ,ORIGINAL CORBONAT MINERALOGY, AND RECONSTRUCTION OF SEDIMENTARY,” JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY), vol. 2, no. 3-4, pp. 63–87, 2003, [Online]. Available: https://sid.ir/paper/44095/en

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