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Magmatic-hydrothermal Transition in the Tanco Rare-element Pegmatite: Evidence from Fluid Inclusions and Phase-equilibrium Experiments.

Authors
London-D
Source
Am Mineral 1986 71:376-395
Link
NIOSHTIC No.
10011766
Abstract
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.
Publication Date
19860101
Document Type
IH; Final Contract Report;
Fiscal Year
1986
Identifying No.
MIR 4-87
NIOSH Division
WO;
Source Name
Am. Mineral., V. 71, 1986, PP. 376-395
State
OK;
Performing Organization
University of Oklahoma
Page last reviewed: March 11, 2019
Content source: National Institute for Occupational Safety and Health Education and Information Division