STUDY OF ORIGINAL CARBONATE MINERALOGY OF THE NAYBAND FORMATION USING GEOCHEMICAL EVIDENCES IN DARBIDKHOON, TARZ, GITRY AND KUHBANAN STRATIGRAPHIC SECTIONS, SE OF IRAN

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KALANTARZADEH Z.; ADABI M.H.; RAHIMPOUR BONAB H.

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Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2015 | Volume:24 | Issue:94 (STRATIGRAPHY & SEDIMENTOLOGY) Page(s): 203-216

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Title

STUDY OF ORIGINAL CARBONATE MINERALOGY OF THE NAYBAND FORMATION USING GEOCHEMICAL EVIDENCES IN DARBIDKHOON, TARZ, GITRY AND KUHBANAN STRATIGRAPHIC SECTIONS, SE OF IRAN

Author(s)

KALANTARZADEH Z. | ADABI M.H. | RAHIMPOUR BONAB H. | Issue Writer Certificate

Keywords

ORIGINAL CARBONATE MINERALOGYQ2

OXYGEN AND CARBON ISOTOPEQ2

GEOCHEMISTRYQ2

NAYBAND FORMATIONQ2

Abstract

After Early Cimmerian orogenic stage, due to marine transgression, the NAYBAND FORMATION Norian_Rethian (Upper Triassic) in age deposited in the Central Iran Zone. Because of transforming of aragonite and high Mg calcite into low Mg calcite during diagenesis, recognition of ORIGINAL CARBONATE MINERALOGY based on petrographic studies is difficult. In this research, ORIGINAL CARBONATE MINERALOGY and type of carbonates (tropical, temperate and polar) of the NAYBAND FORMATION in Darbidkhoon, Tarz, Gitry and Kuhbanan stratigraghic sections have been studied using geochemical evidences. The trace elements (Na, Sr, Fe, Mn) and isotopes (and) data of the NAYBAND FORMATION carbonates is located inside or close to the aragonitic tropical Fahlian Formation (Lower Cretaceous), the Ilam Formation (Upper Cretaceous), the Kangane Formation (Lower Triassic) and the Mozduran Formation (Upper Jurassic) limestones, because of aragonitic ORIGINAL CARBONATE MINERALOGY. The results of elemental and isotopic analysis correlate with the petrographic evidences and paleogeographic map of the Upper Triassic.

Cites

CRUZIANA ICHNOFACIES FROM NAYBAND FORMATION (LATE TRIASSIC) IN THE PARVADEH SECTION, SOUTHWEST TABAS, EAST CENTRAL IRAN

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APA: Copy

KALANTARZADEH, Z., ADABI, M.H., & RAHIMPOUR BONAB, H.. (2015). STUDY OF ORIGINAL CARBONATE MINERALOGY OF THE NAYBAND FORMATION USING GEOCHEMICAL EVIDENCES IN DARBIDKHOON, TARZ, GITRY AND KUHBANAN STRATIGRAPHIC SECTIONS, SE OF IRAN. GEOSCIENCES, 24(94 (STRATIGRAPHY & SEDIMENTOLOGY)), 203-216. SID. https://sid.ir/paper/32168/en

Vancouver: Copy

KALANTARZADEH Z., ADABI M.H., RAHIMPOUR BONAB H.. STUDY OF ORIGINAL CARBONATE MINERALOGY OF THE NAYBAND FORMATION USING GEOCHEMICAL EVIDENCES IN DARBIDKHOON, TARZ, GITRY AND KUHBANAN STRATIGRAPHIC SECTIONS, SE OF IRAN. GEOSCIENCES[Internet]. 2015;24(94 (STRATIGRAPHY & SEDIMENTOLOGY)):203-216. Available from: https://sid.ir/paper/32168/en

IEEE: Copy

Z. KALANTARZADEH, M.H. ADABI, and H. RAHIMPOUR BONAB, “STUDY OF ORIGINAL CARBONATE MINERALOGY OF THE NAYBAND FORMATION USING GEOCHEMICAL EVIDENCES IN DARBIDKHOON, TARZ, GITRY AND KUHBANAN STRATIGRAPHIC SECTIONS, SE OF IRAN,” GEOSCIENCES, vol. 24, no. 94 (STRATIGRAPHY & SEDIMENTOLOGY), pp. 203–216, 2015, [Online]. Available: https://sid.ir/paper/32168/en

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