GEOCHEMISTRY AND PETROLOGY OF NE NARAGH VOLCANIC ROCKS: ISLAND ARC OR ACTIVE CONTINENTAL MARGIN MAGMATISM?

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SHAHRIARI SH.; GHORBANI M.R.; NASIRI BEZENJANI R.

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Journal: Iranian Journal of Crystallography and Mineralogy Year:2011 | Volume:19 | Issue:2 Page(s): 251-262

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Information Journal Paper

Title

GEOCHEMISTRY AND PETROLOGY OF NE NARAGH VOLCANIC ROCKS: ISLAND ARC OR ACTIVE CONTINENTAL MARGIN MAGMATISM?

Author(s)

SHAHRIARI SH. | GHORBANI M.R. | NASIRI BEZENJANI R. | Issue Writer Certificate

Keywords

GEOCHEMISTRYQ2

PETROLOGYQ2

VOLCANIC ROCKSQ2

ISLAND ARCQ2

ACTIVE CONTINENTAL MARGINQ3

NARAGHQ2

Abstract

The tectonic settings for the Urumieh-Dokhtar volcanic-plutonic belt provided by different reaserchers including ACTIVE CONTINENTAL MARGIN rift and post collisional settings.Geochemical and tectonic studies indicate that this belt belongs to the ACTIVE CONTINENTAL MARGIN.Basaltic andesite, andesite, trachy andesite, trachy dacite and dacitic rocks in NE NARAGH, of the Urumieh-Dokhtar magmatic arc, Eocene in age, show some affinities to the volcanic ISLAND ARC, in terms of GEOCHEMISTRY of major and trace elements. In comparison with the ISLAND ARCs (e.g. Marianna) and ACTIVE CONTINENTAL MARGIN (e.g. the Andes), these rocks demonstrate intermediate characteristics. Specific tectonic setting and low thickness of the lithosphere of Central Iran during subduction of the Neo-Tethyan oceanic crust, is the main reason that resulted in the NE NARAGH VOLCANIC ROCKS with geochemical similarities to the ISLAND ARCs.

Cites

GEOCHEMISTRY AND PETROGENESIS OF THE CHEHELTAN MOUNTAIN VOLCANIC ROCKS; SOUTH-WEST OF BARDSIR (KERMAN PROVINCE)

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APA: Copy

SHAHRIARI, SH., GHORBANI, M.R., & NASIRI BEZENJANI, R.. (2011). GEOCHEMISTRY AND PETROLOGY OF NE NARAGH VOLCANIC ROCKS: ISLAND ARC OR ACTIVE CONTINENTAL MARGIN MAGMATISM?. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 19(2), 251-262. SID. https://sid.ir/paper/4084/en

Vancouver: Copy

SHAHRIARI SH., GHORBANI M.R., NASIRI BEZENJANI R.. GEOCHEMISTRY AND PETROLOGY OF NE NARAGH VOLCANIC ROCKS: ISLAND ARC OR ACTIVE CONTINENTAL MARGIN MAGMATISM?. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2011;19(2):251-262. Available from: https://sid.ir/paper/4084/en

IEEE: Copy

SH. SHAHRIARI, M.R. GHORBANI, and R. NASIRI BEZENJANI, “GEOCHEMISTRY AND PETROLOGY OF NE NARAGH VOLCANIC ROCKS: ISLAND ARC OR ACTIVE CONTINENTAL MARGIN MAGMATISM?,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 19, no. 2, pp. 251–262, 2011, [Online]. Available: https://sid.ir/paper/4084/en

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