Abstract
Methodology is described in this paper for investigating biotite reactions in pneumatolyto-hydrothermal solutions rich in Na, F and Li by using tow buffer systems, NNO and CFG. The results show: (1) Under the experimental conditions biotite is unstable and different new stable phases will be formed, depending upon the fugacity of oxygen. Na-rich minerals, such as aegirine and albite, will be produced at low oxygen fugacity, while Li-rich micas are found stable at high oxygen fugacity. This agrees with the field observation that albitization occurs in general at a lower position than that of Li-rich micas, suggesting that alkalimetasomatism of biotite may provide the necessary components for subsequent reactions. (2) The stability of Li-rich micas is dependent on Mg2+ concentration in the medium, which in turn is determined by Mg2+ content in the starting biotite. Li-rich micas are favored by metasomatism of only those biotites that are poor in Mg2+. (3) Unstability of biotite would favor the incorporation of ore-forming elements contained in it as isomorphous impurities into solutions.
Similar content being viewed by others
References
Wones, D.R. and Eugster, H.P.,Amer. Miner., 50(1965), 1228.
Forster, M.D.,U.S.Geol. Surv. Professor Papers, 354-E(1960), 115–146.
Munoz, J.L. and Eugster, H.P.,Amer. Miner., 54, 5–6(1969), 943.
Rieder, M.,Contr. Mineral. and Petrol., 27(1970), 131–158.
Wang Yurong et al.,Geochimica, 1(1981), 95–103(in Chinese).
Frantz, J.D. and Robert, K.P., «Annual Report of the Director Geophysical Laboratory», 1977–1978, 812.
Gu Xiongfei and Xu Yingnian,Geochimica, 2(1973), 61–75(in Chinese).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Yunmei, Y., Yurong, W. An experimental study of biotite in Na-, F-, and Li-rich pneumatolyto-hydrothermal solutions. Chin. J. of Geochem. 7, 76–87 (1988). https://doi.org/10.1007/BF02840432
Issue Date:
DOI: https://doi.org/10.1007/BF02840432