MINERALOGY AND PETROGRAPHY OF CALC-SILICATE XENOLITHS

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KHALILI M.; MAKIZADEH M.A.

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Journal Paper

Paper Information

Journal: Iranian Journal of Crystallography and Mineralogy Year:2004 | Volume:12 | Issue:1 Page(s): 39-50

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Information Journal Paper

Title

MINERALOGY AND PETROGRAPHY OF CALC-SILICATE XENOLITHS

Author(s)

KHALILI M. | MAKIZADEH M.A. | Issue Writer Certificate

Keywords

CALC-SILICATEQ4

MELILITEQ4

XENOLITHQ2

SHIR- KUHQ3

Abstract

The CALC-SILICATE XENOLITHs, within the Shir-Kuh batholith are characterized by MELILITE, garnet, vesuvianite, and wollastonite mineral assemblage. On the basis of paragenetic relations, prograde and retrograde metamorphism are involved in the formation of these minerals. MELILITE, wollastonite and diopside formed during progressive metamorphism which was accompanied by thermal peak shocking and decarbonization reactions in pyroxene-hornfels faces. The effect of fluids in later stage, which released during crystallization of batholith, caused the formation of hydrous minerals (hornblende-hornfels facies during retrograding metamoephism.

Cites

GARNET GENESIS IN ALTERED CONGLOMERATE OF SANGESTAN FORMATION, DAMAK ALIABAD (WEST OF TAFT, YAZD PROVINCE)

References

دیباچه ای بر زمین شناسی ایران

Cite

APA: Copy

KHALILI, M., & MAKIZADEH, M.A.. (2004). MINERALOGY AND PETROGRAPHY OF CALC-SILICATE XENOLITHS. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 12(1), 39-50. SID. https://sid.ir/paper/3806/en

Vancouver: Copy

KHALILI M., MAKIZADEH M.A.. MINERALOGY AND PETROGRAPHY OF CALC-SILICATE XENOLITHS. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2004;12(1):39-50. Available from: https://sid.ir/paper/3806/en

IEEE: Copy

M. KHALILI, and M.A. MAKIZADEH, “MINERALOGY AND PETROGRAPHY OF CALC-SILICATE XENOLITHS,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 12, no. 1, pp. 39–50, 2004, [Online]. Available: https://sid.ir/paper/3806/en

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