GEOCHEMICAL MODELING OF PARTIAL MELTING ON THE TALL-E-PAHLEVANI MIGMATITIC XENOLITHS, SHAHR-E-BABAK

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FAZLNIA ABDOLNASER

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Journal: PETROLOGY Year:2010 | Volume:1 | Issue:1 Page(s): 11-26

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Title

GEOCHEMICAL MODELING OF PARTIAL MELTING ON THE TALL-E-PAHLEVANI MIGMATITIC XENOLITHS, SHAHR-E-BABAK

Author(s)

FAZLNIA ABDOLNASER | Issue Writer Certificate

Keywords

GEOCHEMICAL MODELINGQ3

PARTIAL MELTINGQ2

MIGMATITEQ2

METAPELITEQ2

REEQ1

Abstract

Falling down of pieces of garnet-biotite-kyanite schists from the Qori metamorphic complex (southern part of Sanandaj-Sirjan zone, northeast Neyriz) into the Tall-e-Pahlevani intrusion, with an initial composition of leuco-quartz diorite–anorthosite, led to these schists (xenoliths) undergo highly contact metamorphic degrees up to pyroxene hornfels facies, and hence were formed felsic MIGMATITEs. Melt volume size produced (leucosome) based on minor element GEOCHEMICAL MODELING was about 50 to 70 vol. %. Some parts of the partial melts (probably <25 vol. %) were extracted from the xenoliths, joined each other, and produced small patches of the per-aluminous granites.

Cites

GEOCHEMICAL MODELING OF PARTIAL MELTING ON THE TALL-E-PAHLEVANI MIGMATITIC XENOLITHS, SHAHR-E-BABAK

References

GEOCHEMICAL MODELING OF PARTIAL MELTING ON THE TALL-E-PAHLEVANI MIGMATITIC XENOLITHS, SHAHR-E-BABAK

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APA: Copy

FAZLNIA, ABDOLNASER. (2010). GEOCHEMICAL MODELING OF PARTIAL MELTING ON THE TALL-E-PAHLEVANI MIGMATITIC XENOLITHS, SHAHR-E-BABAK. PETROLOGY, 1(1), 11-26. SID. https://sid.ir/paper/196939/en

Vancouver: Copy

FAZLNIA ABDOLNASER. GEOCHEMICAL MODELING OF PARTIAL MELTING ON THE TALL-E-PAHLEVANI MIGMATITIC XENOLITHS, SHAHR-E-BABAK. PETROLOGY[Internet]. 2010;1(1):11-26. Available from: https://sid.ir/paper/196939/en

IEEE: Copy

ABDOLNASER FAZLNIA, “GEOCHEMICAL MODELING OF PARTIAL MELTING ON THE TALL-E-PAHLEVANI MIGMATITIC XENOLITHS, SHAHR-E-BABAK,” PETROLOGY, vol. 1, no. 1, pp. 11–26, 2010, [Online]. Available: https://sid.ir/paper/196939/en

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