MINERALOGY, PARAGENESIS, TEXTURE AND MINERAL FACIES OF SKARNS IN WEST OF MALAYER

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VEISKARAMI H.; RASHIDNEJAD OMRAN N.; GHADERI M.

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Journal: Iranian Journal of Crystallography and Mineralogy Year:2013 | Volume:20 | Issue:4 Page(s): 701-712

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Information Journal Paper

Title

MINERALOGY, PARAGENESIS, TEXTURE AND MINERAL FACIES OF SKARNS IN WEST OF MALAYER

Author(s)

VEISKARAMI H. | RASHIDNEJAD OMRAN N. | GHADERI M. | Issue Writer Certificate

Keywords

METAMORPHIC FACIESQ2

PARAGENESISQ2

MINERALOGYQ2

FABRICSQ2

SKARNQ2

WEST OF MALAYERQ2

Abstract

Triassic (mostly volcanic-carbonate) and Jurassic (mainly shale and sandstone) rocks in WEST OF MALAYER were affected by a number of shear zone, folding, deformation and metamorphic events. Regional metamorphism in the area led to the formation of Triassic and Jurassic rocks such as phyllite, slate and crystalline carbonate which folded during deformational events. In the contact metamorphism event, granitoid plutons with predominantly granodiorite to quartz-diorite composition intruded the metamorphic rocks, forming mineralized SKARN zones in Anjireh, Iraneh and SarabSaman areas. The present research shows that plutons producing the mineralized SKARN zones in the area are on average granodioritic in composition.Pyroxene and garnet minerals in the SKARN zone comprise of diopside, augite and grandite (mainly andradite), respectively. In these SKARNs, various sub-zones are recognized and defined on the basis of their mineral PARAGENESIS. High temperature facies (pyroxene-fels) formed in the temperature range of 650-800 oC and wollastonite up to 800 oC. However, hornblende-fels and albite-epidote-fels facies formed in the temperature ranges 500-650 and 350-500 oC, respectively.

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References

مطالعه کانی شناسی و سنگ شناسی گرانودیوریت سامن (ملایر)

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APA: Copy

VEISKARAMI, H., RASHIDNEJAD OMRAN, N., & GHADERI, M.. (2013). MINERALOGY, PARAGENESIS, TEXTURE AND MINERAL FACIES OF SKARNS IN WEST OF MALAYER. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 20(4), 701-712. SID. https://sid.ir/paper/4056/en

Vancouver: Copy

VEISKARAMI H., RASHIDNEJAD OMRAN N., GHADERI M.. MINERALOGY, PARAGENESIS, TEXTURE AND MINERAL FACIES OF SKARNS IN WEST OF MALAYER. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2013;20(4):701-712. Available from: https://sid.ir/paper/4056/en

IEEE: Copy

H. VEISKARAMI, N. RASHIDNEJAD OMRAN, and M. GHADERI, “MINERALOGY, PARAGENESIS, TEXTURE AND MINERAL FACIES OF SKARNS IN WEST OF MALAYER,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 20, no. 4, pp. 701–712, 2013, [Online]. Available: https://sid.ir/paper/4056/en

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