Abstracts for Annual Meeting of Japan Association of Mineralogical Sciences
2018 Annual Meeting of Japan Association of Mineralogical Sciences
Session ID : R8-07
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R8: Metamorphic rocks and tectonics
Significance of tourmaline-bearing nanogranite inclusions in garnet from High Himalayan Crystalline sequence, central Nepal
*Tetsuo KawakamiHarutaka SakaiKatsushi SatoYasuhiro Monta
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Abstract
Tourmaline-bearing nanogranite inclusions (NIs) are found from the pelitic gneiss collected from the Marsyangdi river area, Nepal Himalayas. Garnet has a rim defined by the discontinuous zoning in Ca and P. The NIs are included throughout the garnet core. ~100μm-sized NIs are composed of Bt+Tur+Chl+Pl+Qtz and Bt+Pl+Qtz, whereas several 10μm-sized NIs are composed of Bt+Ms+Qtz±Chl, etc. Tur-bearing NI is a direct evidence of the presence of B-bearing melt, segregation and ascent of which probably formed the High Himalayan leucogranite bodies.
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© 2018 Japan Association of Mineralogical Sciences
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