PETROLOGY AND GEOCHEMISTRY OF QUARTZ-MONZONITE BODY IN THE TAROM SUBZONE NORTH-EAST OF ZANJAN

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NAZARI NIA ASMA; RASHIDNEJAD OMRAN NEMATOLLAH; AGHAZADEH MAHRAJ; ARVIN MOHSEN

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Journal: PETROLOGY Year:2015 | Volume:5 | Issue:20 Page(s): 91-105

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Information Journal Paper

Title

PETROLOGY AND GEOCHEMISTRY OF QUARTZ-MONZONITE BODY IN THE TAROM SUBZONE NORTH-EAST OF ZANJAN

Author(s)

NAZARI NIA ASMA | RASHIDNEJAD OMRAN NEMATOLLAH | AGHAZADEH MAHRAJ | ARVIN MOHSEN | Issue Writer Certificate

Keywords

QUARTZ MONZONITEQ1

GEOCHEMISTRYQ2

PETROLOGYQ2

TAROM OLIAQ2

ZANJANQ1

ALBORZ-AZARBAIJAN ZONEQ1

Abstract

The TAROM OLIA quartz monzonitic intrusive is one of the plutons cropped out in ALBORZ-AZARBAIJAN ZONE which is elongated in NW-SE direction. The pluton, lithologically comprises monzodiorite, monzonite, QUARTZ MONZONITE and monzogranite. Field and petrological studies as well as geochemical considerations revealed that this pluton crystallized from an I-type metaluminous magma with shoshonitic affinity. The magma has originated by melting of a metasomatized lithospheric mantle then affected by processes by which modified composition of the primary magma to produce the intermediate and felsic rocks.

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APA: Copy

NAZARI NIA, ASMA, RASHIDNEJAD OMRAN, NEMATOLLAH, AGHAZADEH, MAHRAJ, & ARVIN, MOHSEN. (2015). PETROLOGY AND GEOCHEMISTRY OF QUARTZ-MONZONITE BODY IN THE TAROM SUBZONE NORTH-EAST OF ZANJAN. PETROLOGY, 5(20), 91-105. SID. https://sid.ir/paper/196945/en

Vancouver: Copy

NAZARI NIA ASMA, RASHIDNEJAD OMRAN NEMATOLLAH, AGHAZADEH MAHRAJ, ARVIN MOHSEN. PETROLOGY AND GEOCHEMISTRY OF QUARTZ-MONZONITE BODY IN THE TAROM SUBZONE NORTH-EAST OF ZANJAN. PETROLOGY[Internet]. 2015;5(20):91-105. Available from: https://sid.ir/paper/196945/en

IEEE: Copy

ASMA NAZARI NIA, NEMATOLLAH RASHIDNEJAD OMRAN, MAHRAJ AGHAZADEH, and MOHSEN ARVIN, “PETROLOGY AND GEOCHEMISTRY OF QUARTZ-MONZONITE BODY IN THE TAROM SUBZONE NORTH-EAST OF ZANJAN,” PETROLOGY, vol. 5, no. 20, pp. 91–105, 2015, [Online]. Available: https://sid.ir/paper/196945/en

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