Ague J J. 2011. Extreme channelization of fluid and the problem of element mobility during Barrovian metamorphism[J]. American Mineralogist, 96: 333-352.
[29]
Brauhart C W, Huston D L, Groves D I, Mikucki E J and Gardoll A S. 2001. Geochemical mass-transfer patterns as indicators of the Architecture of a complete volcanic-hosted massive sulfide hydrothermal alteration system, Panorama district, Pilbara, Western Australia[J]. Econ. Geol., 96: 1263-1278.
[30]
Derakhshani R and Abdolzadeh M. 2009. Mass change calculation during hydrothermal alteration/mineralization in the porphyry copper deposit of Darrehzar, Iran[J]. Research Journal of Environmental Sciences, 3(1): 41-51.
[31]
Grant J A. 1986. The isocon diagram-a simple solution to Gresens equation for metasomatic alteration[J]. Econ. Geol., 81: 1976-1982.
[32]
Grant J A. 2005. Isocon analysis: A brief review of the method and applications[J]. Physics and Chemistry of the Earth, 30: 997-1004.
[33]
Gresens R L. 1967. Composition-volume relation ships of metasomatism[J]. Chemistry Geology, 2: 47-55.
[34]
MacLean W H and Kranidiotis P. 1987. Immobile elements as monitors of mass transfer in hydrothermal alteration: Phelps Dodge massive sulfide deposit, Matagami, Quebec[J]. Econ. Geol., 82:951-962.
[35]
MacLean W H, Bonavia F F and Sanna G. 1997. Argillite debris converted to bauxite during Karst weathering: Evidence from immobile element geochemistry at the Olmedo deposit, Sardinia[J]. Mine-ralium Deposita, 32: 607-616.
[36]
O\'Hara K. 1988. Fluid flow and volume loss during mylonitizion: An origin for phyllonite in an overthrust setting, North Caralia USA[J]. Tectonophysics, 156:21-36.
[37]
Riverin G and Hodgson C J. 1980. Wall-rock alteration at the Millenbach Cu-Zn mine, Noranda[J]. Econ. Geol., 75: 424-444.
[38]
Sinha A K, Hewitt D A and Rimstidt J D. 1986. Fluid interaction and element mobility in the development of ultramylonites[J]. Geology, 14: 883-886.