Based on homogenization temperature and duration of homogenization process obtained from Johannes (DH=r2/4t) and Eyring equations (DN=KB·T /η·λ), the authors calculated the viscosity of a melt inclusion at homogenization. The water content of the inclusion melt was estimated from the experimental diagram LnDH-1/T for granitic melt with different water contents. The study on mineral inclusions from Luanjiahe granite in Jiaodong gold zone indicates that the melt inclusion has a homogenization temperature of 970℃, viscosity of 3.8×106 Pa·s and water content of 2.5%, whereas the fluid_melt inclusion has a homogenization temperature of 855℃, viscosity of 617.7 Pa·s and water content of 5.8%, suggesting that during the crystallization of granitic magma water content increased while viscosity decreased continuously, and at the late stage of crystallization the fluid was close to the saturation state.
Reference
Related
Cited by
Get Citation
曲晓明,王鹤年,王海芹,1998,栾家河花岗岩体中的矿物包裹体研究[J].岩石矿物学杂志,17(3):270~274. Qu Xiaoming,1998,A Study of Mineral Inclusions from Luanjiahe Granite Body[J]. Acta Petrologica et Mineralogica,17(3):270~274.