THE STUDY OF GEOCHEMISTRY AND TECTONIC ENVIRONMENT OF GRANITOID BODIES IN THE WEST OF SAMEN, SOUTH OF AVARZAMAN) WESTERN MALAYER) BASED ON WHOLE ROCK AND CHEMISTRY OF BIOTITE

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RAMOOZ PARVANEH; ZAREI SAHAMIEH REZA; MASORI NEDA

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Journal: GEOCHEMISTRY Year:2014 | Volume:3 | Issue:3 Page(s): 0-0

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Title

THE STUDY OF GEOCHEMISTRY AND TECTONIC ENVIRONMENT OF GRANITOID BODIES IN THE WEST OF SAMEN, SOUTH OF AVARZAMAN) WESTERN MALAYER) BASED ON WHOLE ROCK AND CHEMISTRY OF BIOTITE

Author(s)

RAMOOZ PARVANEH | ZAREI SAHAMIEH REZA | MASORI NEDA | Issue Writer Certificate

Keywords

GRANITOIDQ2

CALC-ALKALINEQ2

PERALUMINOUSQ2

VOLCANIC ARCQ2

SANANDAJ-SIRJANQ2

AVARZAMANQ2

Abstract

The south AVARZAMAN GRANITOID pluton with Cretaceous age is located in the west of Malayer. From tectonic point of view it is a part of plutonism events of SANANDAJ-SIRJAN zone. In this region, injection of this pluton into the Upper Triassic-Lower Jurassic sediments with low metamorphic grade, caused the generation of metamorphic halo which includes the Hornfels and Skarn mineralization. According to the petrography and field evidences, the main rocks of this pluton is made up of medium to coarse-grained granodiorite, monzogranite and quartzodiorite rocks with a lesser amount of tonalite and syeno-granitic type. Several aplitic and quartzitic dykes cut the plutonic and host rocks. Dominant texture of these rocks is granular and porphyroid. The whole rock and minerals such as biotite analysis was used for geochemistry and the tectonic setting showing the same results. Chemically, magma of these rocks is a high-K CALC-ALKALINE suite. Considering the saturation degree of aluminum, it ranges from PERALUMINOUS to a little metaluminous and shows mostly S-type nature but also some tendency to I-type. The GRANITOID pluton in this area, by using composition of biotite, displays CALC-ALKALINE and PERALUMINOUS nature with VOLCANIC ARC tectonic setting. Since the samples are enriched in LREE more than HREE and show depletion of some elements such as Ti, P, Sr, Nb, besides of locating in the range of VAG, this GRANITOID pluton is supposed to be created in a VOLCANIC ARC setting in response to the subduction of Neothetys oceanic crust beneath the Iranian plate.

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APA: Copy

RAMOOZ, PARVANEH, ZAREI SAHAMIEH, REZA, & MASORI, NEDA. (2014). THE STUDY OF GEOCHEMISTRY AND TECTONIC ENVIRONMENT OF GRANITOID BODIES IN THE WEST OF SAMEN, SOUTH OF AVARZAMAN) WESTERN MALAYER) BASED ON WHOLE ROCK AND CHEMISTRY OF BIOTITE. GEOCHEMISTRY, 3(3), 0-0. SID. https://sid.ir/paper/409667/en

Vancouver: Copy

RAMOOZ PARVANEH, ZAREI SAHAMIEH REZA, MASORI NEDA. THE STUDY OF GEOCHEMISTRY AND TECTONIC ENVIRONMENT OF GRANITOID BODIES IN THE WEST OF SAMEN, SOUTH OF AVARZAMAN) WESTERN MALAYER) BASED ON WHOLE ROCK AND CHEMISTRY OF BIOTITE. GEOCHEMISTRY[Internet]. 2014;3(3):0-0. Available from: https://sid.ir/paper/409667/en

IEEE: Copy

PARVANEH RAMOOZ, REZA ZAREI SAHAMIEH, and NEDA MASORI, “THE STUDY OF GEOCHEMISTRY AND TECTONIC ENVIRONMENT OF GRANITOID BODIES IN THE WEST OF SAMEN, SOUTH OF AVARZAMAN) WESTERN MALAYER) BASED ON WHOLE ROCK AND CHEMISTRY OF BIOTITE,” GEOCHEMISTRY, vol. 3, no. 3, pp. 0–0, 2014, [Online]. Available: https://sid.ir/paper/409667/en

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