GEOCHEMICAL EVIDENCE FOR RECOGNITION OF ORIGINAL CARBONATE MINERALOGY OF THE SARVAK, SURGAH AND ILAM FORMATIONS IN SHIVAND SECTION MONGASHT ANTICLINE

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GHALAVAND HORMOZ; SADEGHI ABAS; SHEMIRANI A.; ADAABI M.H.

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Journal: JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT) Year:2009 | Volume:35 | Issue:2 (SECTION: GEOLOGY) Page(s): 51-62

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Title

GEOCHEMICAL EVIDENCE FOR RECOGNITION OF ORIGINAL CARBONATE MINERALOGY OF THE SARVAK, SURGAH AND ILAM FORMATIONS IN SHIVAND SECTION MONGASHT ANTICLINE

Author(s)

GHALAVAND HORMOZ | SADEGHI ABAS | SHEMIRANI A. | ADAABI M.H. | Issue Writer Certificate

Keywords

ORIGINAL CARBONATE MINERALOGYQ3

MAJOR AND MINOR ELEMENTSQ3

CARBON AND OXYGEN ISOTOPESQ3

MONGASHT ANTICLINEQ3

BANGESTAN GROUPQ3

IZEH ZONEQ3

Abstract

Sarvak, Surgah and Ilam Formations from BANGESTAN GROUP with Cenomanian to Santonian age consist of carbonate units and have a total thickness of 679 m in MONGASHT ANTICLINE, Shivand area, 45 km southeast of Izeh, in Zagros basin.Recognition of ORIGINAL CARBONATE MINERALOGY based on petrographic evidence is difficult, because aragonite and high Mg calcite transformed to low Mg calcite during diagenesis.Major (Ca, Mg) and minor elements (Sr, Na, Fe, Mn) and carbon and oxygen isotope values used to determine carbonate mineralogy in Sarvak, Surgah and Ilam Formations. Bivariate plots of MAJOR AND MINOR ELEMENTS and oxygen and carbon isotopes values indicate that aragonite is the ORIGINAL CARBONATE MINERALOGY in studied formations. MAJOR AND MINOR ELEMENTS and oxygen and carbon isotopes values along stratigraphic columns were used to distinguish between Sarvak, Surgah and Ilam Formations.Paleotemperature calculation based on oxygen isotope values of the least altered samples indicate that sea water temperature during precipitations of Sarvak, Surgah and Ilam Formations were 27oC (-3.49 ‰PDB), 31oC (-4.40 ‰PDB), 26oC (-3.21‰PDB) respectively.

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APA: Copy

GHALAVAND, HORMOZ, SADEGHI, ABAS, SHEMIRANI, A., & ADAABI, M.H.. (2009). GEOCHEMICAL EVIDENCE FOR RECOGNITION OF ORIGINAL CARBONATE MINERALOGY OF THE SARVAK, SURGAH AND ILAM FORMATIONS IN SHIVAND SECTION MONGASHT ANTICLINE. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), 35(2 (SECTION: GEOLOGY)), 51-62. SID. https://sid.ir/paper/2138/en

Vancouver: Copy

GHALAVAND HORMOZ, SADEGHI ABAS, SHEMIRANI A., ADAABI M.H.. GEOCHEMICAL EVIDENCE FOR RECOGNITION OF ORIGINAL CARBONATE MINERALOGY OF THE SARVAK, SURGAH AND ILAM FORMATIONS IN SHIVAND SECTION MONGASHT ANTICLINE. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT)[Internet]. 2009;35(2 (SECTION: GEOLOGY)):51-62. Available from: https://sid.ir/paper/2138/en

IEEE: Copy

HORMOZ GHALAVAND, ABAS SADEGHI, A. SHEMIRANI, and M.H. ADAABI, “GEOCHEMICAL EVIDENCE FOR RECOGNITION OF ORIGINAL CARBONATE MINERALOGY OF THE SARVAK, SURGAH AND ILAM FORMATIONS IN SHIVAND SECTION MONGASHT ANTICLINE,” JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), vol. 35, no. 2 (SECTION: GEOLOGY), pp. 51–62, 2009, [Online]. Available: https://sid.ir/paper/2138/en

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