ZARIGAN GRANITE, MAGMATIC OR METASOMATIC?

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GOLKARAM S.; RASHIDNEJAD OMRAN N.; MASOUDI F.; VAHABZADEH GH.

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Paper Information

Journal: JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY) Year:2010 | Volume:10 | Issue:2 Page(s): 825-840

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Information Journal Paper

Title

ZARIGAN GRANITE, MAGMATIC OR METASOMATIC?

Author(s)

GOLKARAM S. | RASHIDNEJAD OMRAN N. | MASOUDI F. | VAHABZADEH GH. | Issue Writer Certificate

Keywords

ZARIGAN GRANITEQ3

METASOMATISMQ2

HYDROTHERMAL DIFFERENTIATIONQ3

LEUCOCRATQ3

CENTRAL IRANQ3

NORTH OF BAFGHQ3

Abstract

Zarigan and Chah-Chole granite bodies located at the NORTH OF BAFGH, southeastern Ardakan 1:250000 map, part of CENTRAL IRAN microcontinent. These bodies vary compositionally from alkali- feldspar granite to syeno- monzo granite. They are LEUCOCRAT and subvolcanic, mineralogically mainly quartz- feldspathic with lack of mafic minerals. Various textures of magmatic, deformation, metasomatic, granophyric, graphic, mylonitic, cataclastic, myrmekitic, pertitic and replacement can be found in these granites. Geochemically these bodies indicate calkalkaline to alkaline, peraluminous I-type characteristics and magmatic arc geoenviroment. They show different elemental behavior within variation diagrams, based on affinity, mobility and compatibility and intensity of tectonic structures and deformation, indicate the influence of both differentiation and metasomatic processes on the bodies. Field observations and petrographic and geochemical evidences on the Zarigan and Chah- Chole bodies indicate that at least part of those had formed from the earlier dioritic and gabbroic and pyroclastic rocks via METASOMATISM and HYDROTHERMAL DIFFERENTIATION processes, but after emplacement within the upper levels of the area, they also have been under the influence of these processes. The comparison of these rocks with criteria has been proposed for distinguishing magmatic and metasomatic granites, revealed that they share some characteristic features with magmatic bodies, but of course especially ZARIGAN GRANITE has the most congruency with E-type or metasomatic granite.

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APA: Copy

GOLKARAM, S., RASHIDNEJAD OMRAN, N., MASOUDI, F., & VAHABZADEH, GH.. (2010). ZARIGAN GRANITE, MAGMATIC OR METASOMATIC?. JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY), 10(2), 825-840. SID. https://sid.ir/paper/44051/en

Vancouver: Copy

GOLKARAM S., RASHIDNEJAD OMRAN N., MASOUDI F., VAHABZADEH GH.. ZARIGAN GRANITE, MAGMATIC OR METASOMATIC?. JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY)[Internet]. 2010;10(2):825-840. Available from: https://sid.ir/paper/44051/en

IEEE: Copy

S. GOLKARAM, N. RASHIDNEJAD OMRAN, F. MASOUDI, and GH. VAHABZADEH, “ZARIGAN GRANITE, MAGMATIC OR METASOMATIC?,” JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY), vol. 10, no. 2, pp. 825–840, 2010, [Online]. Available: https://sid.ir/paper/44051/en

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