DETERMINATION OF ORIGINAL CARBONATE MINERALOGY OF ILAM FORMATION AND RECOGNITION OF BOUNDARY BETWEEN ILAM AND SARVAK FORMATIONS BY GEOCHEMICAL DATA IN THE PEYON ANTICLINE, NORTH OF IZEH

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ADAABI M.H.; ASADI MEHMANDOUSTI E.

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Journal: Iranian Journal of Crystallography and Mineralogy Year:2006 | Volume:13 | Issue:2 Page(s): 229-244

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Title

DETERMINATION OF ORIGINAL CARBONATE MINERALOGY OF ILAM FORMATION AND RECOGNITION OF BOUNDARY BETWEEN ILAM AND SARVAK FORMATIONS BY GEOCHEMICAL DATA IN THE PEYON ANTICLINE, NORTH OF IZEH

Author(s)

ADAABI M.H. | ASADI MEHMANDOUSTI E. | Issue Writer Certificate

Keywords

CARBONATE MINERALOGYQ4

MAJOR AND MINOR ELEMENTSQ2

CARBON AND OXYGEN ISOTOPESQ2

DIAGENESISQ2

ILAM FORMATIONQ2

Abstract

The Ham Formation (Santonian-Campanian) is a unit of Bangestan Group, which is overlain on the Sarvak Formation in Tang E-Rashid area, Peyon Anticline (18.5 Km North of Izeh). Due to similar lithology, recognition of the exact boundary between Ham and Sarvak Formations in the study area was difficult. Thus it is not possible to determine boundary between these two formations based on petrographic evidence and field observations. Recognition of original CARBONATE MINERALOGY based on petrographic studies is difficult in ancient carbonate rocks, because aragonite (A) and high -Mg calcite (HMC) transformed to low Mg calcite (LMC) during digenesis. In this study MAJOR AND MINOR ELEMENTS and CARBON AND OXYGEN ISOTOPES values used to determine the original CARBONATE MINERALOGY of Ham Formation in the Peyon Anticline. Bivariet plots of minor and major elements and oxygen and carbon isotopes values indicate that original CARBONATE MINERALOGY was aragonite in Ham Formation. Elemental and isotopic compositions of Ham carbonates also illustrate that they were affected by non-marine digenesis in a closed system. Major and minor element variations (such as Sr, Sr/Ca, and Sr/Na) and oxygen and carbon isotopes were used to distinguish the boundary between Ilam and Sarvak Formations in the Peyon Anticline.

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APA: Copy

ADAABI, M.H., & ASADI MEHMANDOUSTI, E.. (2006). DETERMINATION OF ORIGINAL CARBONATE MINERALOGY OF ILAM FORMATION AND RECOGNITION OF BOUNDARY BETWEEN ILAM AND SARVAK FORMATIONS BY GEOCHEMICAL DATA IN THE PEYON ANTICLINE, NORTH OF IZEH. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 13(2), 229-244. SID. https://sid.ir/paper/4224/en

Vancouver: Copy

ADAABI M.H., ASADI MEHMANDOUSTI E.. DETERMINATION OF ORIGINAL CARBONATE MINERALOGY OF ILAM FORMATION AND RECOGNITION OF BOUNDARY BETWEEN ILAM AND SARVAK FORMATIONS BY GEOCHEMICAL DATA IN THE PEYON ANTICLINE, NORTH OF IZEH. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2006;13(2):229-244. Available from: https://sid.ir/paper/4224/en

IEEE: Copy

M.H. ADAABI, and E. ASADI MEHMANDOUSTI, “DETERMINATION OF ORIGINAL CARBONATE MINERALOGY OF ILAM FORMATION AND RECOGNITION OF BOUNDARY BETWEEN ILAM AND SARVAK FORMATIONS BY GEOCHEMICAL DATA IN THE PEYON ANTICLINE, NORTH OF IZEH,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 13, no. 2, pp. 229–244, 2006, [Online]. Available: https://sid.ir/paper/4224/en

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