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Sajan sarthak
Fluid in magma are very much effective in breaking the bond keeping the magma less viscous . Fluidsids can be Water , carbon dioxide, sulphur,chlorine . Option B,C are eliminated as they are viscous because they are having high sillica( sio2 content) Basaltic glass could also have been the answer but because of less viscocity but that glass term indicates no proper development of grains . but granitic pegmatite clearly shows less viscocity so big grain development due to fast movement of ions to the nucleation site.