DETERMINING PROTOLITH AND METAMORPHIC GRADE FOR BIOTITE-GARNET GNEISS IN THE RUBY RANGE, SW MT
The Ruby Range contains uplifted exposures of Precambrian crystalline basement rocks, which are considered part of the Montana Metasedimentary terrane (MMT) of the NW Wyoming province (Mogk et al., 1992). The Dillon Gneiss is structurally between two other Precambrian metamorphic suites in a west-dipping sequence (James, 1990). The Dillon Gneiss is known to include mylonitized leucogranite with an intrusive age of ~2.43 Ga yielded by U-Pb dating, and pelitic gneisses with metamorphic ages of both ~2.43 and ~1.77 Ga yielded by LASS monazite dating (Baldwin et al., 2017; Baker et al., 2017).
Although some sections of the Ruby Range have been closely studied, the Dillon Gneiss has been neglected because it is a complex, undivided suite of rocks that is volumetrically dominated by quartzofeldspathic gneiss. The BGG was targeted for this study because it is possible to determine the temperature of metamorphism where garnet and biotite occur in equilibrium. Ultimately, the goal is to understand what continental dynamics were in motion in Laurentia during the time of gneiss metamorphism. With this information, understanding how continents are created and then grow from the amalgamation of smaller bodies can continue to expand.