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- W2136871567 abstract "A diverse Precambrian sequence of garnetrich gneisses and schists with lenses of marble, quartzite, iron formation, amphibolite, orthoamphibolite, serpentinite, garnet amphibolite, and aluminous schist occurs in the thin and discontinuous X(A)g map unit (O’Neill et al., 1996) in the southern Highland Mountains of southwestern Montana. This distinctive unit is lithologically similar to sequences in the adjacent Precambrian basement of the Tobacco Root Mountains that were affected by the 1.78 Ga Big Sky orogeny described by Burger, Brady, Cheney and Harms (2004). These similarities may provide a link between these two ranges and offer insight into the extent of the Big Sky orogeny." @default.
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- W2136871567 date "2006-01-01" @default.
- W2136871567 modified "2023-09-27" @default.
- W2136871567 title "METAMORPHISM OF PRECAMBRIAN ROCKS IN THE SOUTHERN HIGHLAND MOUNTAINS, SOUTHWESTERN MONTANA" @default.
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