Testing of sulfide solubility models and calculations of SCSS during crystallization of mafic magmas parental to layered intrusions
1 IntroductionOver the last 20 years, at least ten models for sulfide solubility in silicate melts have been proposed (Ariskin A.A et al., 2008; Boudreau, A.E., and Simon, A. ,2007) These models may be divided to three groups: ① those designed for systems open to sulfur fugacity . ② models based on the sulfur capacity concept (Fincham C. J. B. and Richardson F. D. , 1954), in which the effect of fS2 is accounted for implicitly, and ③ models describing system closed to sulfur, in which the sulfide saturation surface is considered to be a function of melt composition (including S2-), with temperature, pressure and fO2 being external intensive parameters (Holzheid, A. and Grove, T.L., 2002; Li, C, and Ripley, E.M. ,2005; Liu, Y et al., 2007; Mavrogenes, J. A. and ONeill, H. St. C. ,1999).
Kirill Bychkov Alexey Ariskin Leonid Danyushevsky
CODES and School of Earth Sciences, University of Tasmania, Private Bag 79, Hobart, Australia Vernad Vernadsky Institute, Kosygin str., 19, Moscow, Russia CODES and School of Earth Sciences, University of Tasmania, Private Bag 79, Hobart, Australia
国际会议
Xian International Ni-Cu(Pt) Deposit Symposium 2009(2009 西安·Ni-Cu(Pt)岩浆矿床国际学术研讨会)
西安
英文
15-19
2009-09-01（万方平台首次上网日期，不代表论文的发表时间）