A Study of Mineral Inclusions from Luanjiahe Granite Body
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    Abstract:

    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 3.8×106 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.

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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.

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