Magmatic-hydrothermal Transition in the Tanco Rare-element Pegmatite: Evidence from Fluid Inclusions and Phase-equilibrium Experiments.
Am Mineral 1986 71:376-395
This report describes the evaluation of fluid inclusions in petalite, spodumene, eucryptite, and in coexisting quartz with respect to experimentally calibrated reaction relationships in the system lialsio4sio2 to define the cooling path and fluid evolution of the rare-element pegmatite from the Tanco Mine, at Bernic Lake, Manitoba, Canada.
IH; Final Contract Report;
Am. Mineral., V. 71, 1986, PP. 376-395
University of Oklahoma