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Can. Mineral. 40 (5): 1249-1286

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Journal Article
Published: 01 October 2004
The Canadian Mineralogist (2004) 42 (5): 1425–1441.
...) are δ 18 O = −8 to 0‰ and δD = −40 to −5‰ [ www.isohis.iaea.org ]. The mineral deposits of the New Ross area represent a variety of mineralization styles and, as shown by Carruzzo et al. (2000) , their formation involved three roughly coeval reservoirs of fluid. In the conventional δ 18 O – δD...
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Journal Article
Published: 01 May 2016
The Canadian Mineralogist (2016) 54 (3): 737–754.
... of daughter minerals can be used to constrain the composition of the contained fluid and requires accurate identification of the solids as well as data on their solubility and phase equilibria. In particular, in many mineral deposits, halite is the most common daughter mineral in saline liquid-vapor-solid...
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Journal Article
Published: 01 August 2009
The Canadian Mineralogist (2009) 47 (4): 745–764.
... Ma pegmatite–aplite sheets, Peggys Cove, Nova Scotia, Canada . Can. Mineral . 40 , 12491286 . Kontak , D.J. , Farrar , E. , McBride , S. & Martin , R.F. ( 1995 ): Mineral chemistry and 40 Ar/ 39 Ar dating of muscovite from the East Kemptville leucogranite, southern...
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Journal Article
Published: 01 October 2004
The Canadian Mineralogist (2004) 42 (5): 1315–1329.
... from −70° to −20°C, but most of the data are in the range −40° to −25°C ( Fig. 6 ). From the foregoing observations and temperature of last melting of ice and halides, the bulk composition of the fluid is inferred to be 20–45 wt.% equiv. NaCl. However, from the T fm and presence of daughter minerals...
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Journal Article
Published: 01 June 2006
The Canadian Mineralogist (2006) 44 (3): 563–598.
... ) indicates that it is dominated by zones of megacrystic K-feldspar, spodumene, fine-grained albite, and intergranular pegmatite material composed of variable proportions of spodumene – K-feldspar – quartz – muscovite. Further subdivisions can be made on the basis of textures, grain size and mineral...
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Journal Article
Published: 01 April 2011
The Canadian Mineralogist (2011) 49 (2): 417–439.
... and can provide more information about petrogenesis. For instance, the cations present in garnet are sensitive to both pressure and temperature (P–T) conditions during crystallization. Mineral inclusions that are locked in garnet may yield additional P–T information. Garnet also is useful...
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Journal Article
Published: 01 August 2009
The Canadian Mineralogist (2009) 47 (4): 697–724.
...), and melt components dissolved into the vapor phase, thereby lowering the activities of added fluxing components. As the diffusive reaction proceeded, the concentrations of fluxes at the interface waned with time. The diffusion coefficients can be estimated, however, from the relation F ig . 5...
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