MINERALOGY AND GENESIS OF THE MISHDOVAN REFRACTORY ORE BODIES BAFGH, CENTRAL IRAN

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KOHSARY A.H.; MOJTAHEDZADEH S.H.; DEHGHANI AHMADABAD M.

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Journal: IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY Year:2010 | Volume:18 | Issue:2 Page(s): 255-266

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Title

MINERALOGY AND GENESIS OF THE MISHDOVAN REFRACTORY ORE BODIES BAFGH, CENTRAL IRAN

Author(s)

KOHSARY A.H. | MOJTAHEDZADEH S.H. | DEHGHANI AHMADABAD M.

Keywords

MINERALOGYQ2

ANDALUSITEQ2

SILLIMANITEQ3

KYANITEQ2

REFRACTORY MINERALSQ3

SHISTQ1

BAFGH MISHDOVAN MINERAL DEPOSITQ3

Abstract

Bafgh Mishdovan ore body is located in the Central Iranian zone and is recognized as potential of the sillimanite group minerals. In this region, the outcrops of the different formations can be observed which mainly consist of the Precambrian metamorphic rocks. Silimanite group minerals are existed in the schistic rocks. The area is located in a tectonized zone and subjected to regional metamorphism then intruded by igneous plutonic rocks. The study area has 95 km2 coverage and according to quality and grade of sillimanite group minerals can be divided to four different mineral zones. Primary exploration activities have been carried out by digging of the trenches and test pits. Samples were taken systematically from outcrops, trenches and test pits. In order to recognize of the ore body (via mineralogy studies), some samples were sent to the laboratory for thin section studies and also XRD and XRF analysis. Based on these investigations, it is verified that the refractory minerals are consisted of sillimanite and kyanite and rarely andalusite. Based on the hosted rocks type and their metamorphic stages, thin section studies and XRD analysis, the phase transition of the primary and alusite into sillimanite and kyanite due to the high temperature-contact metamorphism can be justified. Also regarding the XRD analysis, only one sample contains some kyanites, so it seems that ore bodies is low grade and beneficiation of this industrial minerals face many difficulties or may not be feasible.

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PROCESSING STUDIES AND EVALUATION OF ECONOMIC POTENTIAL OF ANDALUSITE RESERVES FROM EAST FARIMAN

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APA: Copy

KOHSARY, A.H., MOJTAHEDZADEH, S.H., & DEHGHANI AHMADABAD, M.. (2010). MINERALOGY AND GENESIS OF THE MISHDOVAN REFRACTORY ORE BODIES BAFGH, CENTRAL IRAN. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 18(2), 255-266. SID. https://sid.ir/paper/3974/en

Vancouver: Copy

KOHSARY A.H., MOJTAHEDZADEH S.H., DEHGHANI AHMADABAD M.. MINERALOGY AND GENESIS OF THE MISHDOVAN REFRACTORY ORE BODIES BAFGH, CENTRAL IRAN. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2010;18(2):255-266. Available from: https://sid.ir/paper/3974/en

IEEE: Copy

A.H. KOHSARY, S.H. MOJTAHEDZADEH, and M. DEHGHANI AHMADABAD, “MINERALOGY AND GENESIS OF THE MISHDOVAN REFRACTORY ORE BODIES BAFGH, CENTRAL IRAN,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 18, no. 2, pp. 255–266, 2010, [Online]. Available: https://sid.ir/paper/3974/en

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