Structural elements and stratigraphy of the central Snowcrest Range, southwestern Montana, reflect multiple reactivation of what was probably a late Archean and/or Early Proterozoic collisional margin. The tectonic evolution and geodynamic setting are discussed. -from Authors
CITATION STYLE
McBride, B. C., Schmidt, C. J., Guthrie, G. E., & Sheedlo, M. K. (1993). Multiple reactivation of a collisional boundary: an example from southwestern Montana. Basement Tectonics 8, 341–357. https://doi.org/10.1007/978-94-011-1614-5_23
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