Theoretical studies of the alteration of spodumene, petalite, eucryptite and pollucite in granitic pegmatites: exchange reactions with alkali feldspars

Author:

Wood Scott A.,Williams-Jones Anthony E.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference46 articles.

1. Bennington KO, Beyer RP, Johnson GK (1983) Thermodynamic properties of pollucite (a cesium-aluminum-silicate). US Bur Mines Rep Invest 8779:1?18

2. Brimhall GH, Crerar DA (1987) Ore fluids: Magmatic to supergene In: Carmichael ISE, Eugster HP (eds) Thermodynamic modeling of geological materials: minerals, fluids and melts (Reviews in Minerology Society of America vol. 17). Minerological Washington DC, pp 235?321

3. Burnham CW, Nekvasil H (1986) Equilibrium properties of granite pegmatite magmas. Am Mineral 71:239?263

4. Carron J-P, Lagache M (1980) Etude expérimentale du fractionnement des éléments Rb, Cs, Sr et Ba entre feldspaths alcalins, solutions hydrothermales et liquides silicatés dans le système Q. Ab.Or.H2O à 2 kbar entre 700 et 800°C. Bull Mineral 103:571?578

5. Cerny P (1972) The Tanco Pegmatite at Bernic Lake, Manitoba. VIII. Secondary minerals from the spodumenerich zones. Can Mineral 11:714?726

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