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- Amphibolite -- Montana -- Tobacco Root Mountains (1)
- Aroostook County (1)
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- Geology -- Montana -- Tobacco Root Mountains (1)
- Geomorphology (1)
- Glacial Geology (1)
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- Ice Divides (1)
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- Metamorphism (Geology) -- Montana -- Tobacco Root Mountains (1)
- Metasomatism (Mineralogy) (1)
- Quaternary (1)
- Sedimentary Structures (1)
- Stratigraphy (1)
- Ultrabasic rocks -- Montana -- Tobacco Root Mountains (1)
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Articles 1 - 2 of 2
Full-Text Articles in Mineral Physics
Contributions To The Quaternary Geology Of Northern Maine And Adjacent Canada, J. Steven Kite (Ed.), Thomas V. Lowell (Ed.), Woodrow B. Thompson (Ed.)
Contributions To The Quaternary Geology Of Northern Maine And Adjacent Canada, J. Steven Kite (Ed.), Thomas V. Lowell (Ed.), Woodrow B. Thompson (Ed.)
Maine Collection
Contributions to the Quaternary Geology of Northern Maine and Adjacent Canada
Bulletin 37 - Maine Geological Survey, Department of Conservation,
Augusta, Maine 04333 (1988).
Contents: Introduction / A GEOMORPHIC METHOD FOR RECONSTRUCTING PALEO ICE SHEETS, Part I: GLACIAL GEOLOGY. - T. Hughes and J. Fastook / A GEOMORPHIC METHOD FOR RECONSTRUCTING PALEO ICE SHEETS, Part II: GLACIOLOGY. - J. Fastook and T. Hughes / TILL STRATIGRAPHY AT THE BALD MOUNTAIN MINE SITE, NORTHERN MAINE - W. R. Holland and F. F. Bragdon / GLACIAL DISPERSAL FROM THE PRIESTLY LAKE AND DEBOULLIE PLUTONS, NORTHERN MAINE - E. F. Halter / GLACIATION …
Metasomatism Between Amphibolite And Metaultramafic Rocks During Upper Amphibolite Facies Metamorphism, Tobacco Root Mountains, Southwest Montana, William Robert Mcculloch
Metasomatism Between Amphibolite And Metaultramafic Rocks During Upper Amphibolite Facies Metamorphism, Tobacco Root Mountains, Southwest Montana, William Robert Mcculloch
Dissertations and Theses
The purpose of this study is to characterize the metasomatism that has taken place as a result of the chemical incompatibility between mafic and metaultramafic bulk compositions during high-grade regional metamorphism in the Tobacco Root Mountains, southwest Montana. Metasomatism of these rocks took place by both diffusionand infiltration-dominated processes. The result of these processes are characterized mineralogically and geochemically in the rocks.