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The two olivine-bearing zones of the Middle Banded series of the Stillwater Complex are characterized by an increase in the number of cumulus minerals with height. In each, anorthosite and anorthositic troctolite dominate the lower part whereas olivine gabbro and gabbronorite form much of the upper portions. Electron microprobe analyses of cumulus minerals indicate little or no variation of averag...

Petrology and Mineral Compositions of the Middle Banded Series of the Stillwater Complex, Montana