GEOCHEMICAL, SEDIMENTARY ENVIRONMENT AND DIGENESIS OF CARBONATE ROCKS OF THE ASMARI FORMATION (TYPE SECTION IN TANG-E- GEL TORSH)

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ADAABI M.H.; SHOUSHTARIAN F.A.S.; GHALAVAND HORMOZ

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Paper Information

Journal: JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT) Year:2006 | Volume:32 | Issue:3 (SECTION GEOLOGY 2) Page(s): 189-202

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Title

GEOCHEMICAL, SEDIMENTARY ENVIRONMENT AND DIGENESIS OF CARBONATE ROCKS OF THE ASMARI FORMATION (TYPE SECTION IN TANG-E- GEL TORSH)

Author(s)

ADAABI M.H. | SHOUSHTARIAN F.A.S. | GHALAVAND HORMOZ | Issue Writer Certificate

Keywords

ASMARI FORMATIONQ3

OXYGEN ISOTOPESQ3

CARBON ISOTOPESQ3

PETROGRAPHIC STUDIESQ3

Abstract

The study area is located about 35 km southeast of Masjed Soleyman in Khuzestan province (in Zagros basin). Carbonate rocks of ASMARI FORMATION at Tang-e-Gel Torsh consist of 320 meters of thin bedded limestone with intercalation of marls and I thick to massive bedded grey limestones. Petrographic and facies analysis led to recognition of II microfacies deposited in an open marine, barrier, lagoon and tidal flat environments. Major and minor elements and stable isotopes (oxygen and carbon) suggest original aragonite mineralogy for Asmari.Formation Stable oxygen and carbon as well as major and minor elements such as Sr/Cavs Mnalso show that Asmari carbonates were affected by meteoric digenesis in a semi-close to close system.Pale temperature calculation indicates an average ambient sea water temperature of 24S0 C.

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APA: Copy

ADAABI, M.H., SHOUSHTARIAN, F.A.S., & GHALAVAND, HORMOZ. (2006). GEOCHEMICAL, SEDIMENTARY ENVIRONMENT AND DIGENESIS OF CARBONATE ROCKS OF THE ASMARI FORMATION (TYPE SECTION IN TANG-E- GEL TORSH). JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), 32(3 (SECTION GEOLOGY 2)), 189-202. SID. https://sid.ir/paper/2292/en

Vancouver: Copy

ADAABI M.H., SHOUSHTARIAN F.A.S., GHALAVAND HORMOZ. GEOCHEMICAL, SEDIMENTARY ENVIRONMENT AND DIGENESIS OF CARBONATE ROCKS OF THE ASMARI FORMATION (TYPE SECTION IN TANG-E- GEL TORSH). JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT)[Internet]. 2006;32(3 (SECTION GEOLOGY 2)):189-202. Available from: https://sid.ir/paper/2292/en

IEEE: Copy

M.H. ADAABI, F.A.S. SHOUSHTARIAN, and HORMOZ GHALAVAND, “GEOCHEMICAL, SEDIMENTARY ENVIRONMENT AND DIGENESIS OF CARBONATE ROCKS OF THE ASMARI FORMATION (TYPE SECTION IN TANG-E- GEL TORSH),” JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), vol. 32, no. 3 (SECTION GEOLOGY 2), pp. 189–202, 2006, [Online]. Available: https://sid.ir/paper/2292/en

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