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Geology, age, and tectonic setting of the Cretaceous Sliderock Mountain Volcano, Montana
The Sliderock Mountain stratovolcano, part of the Upper Cretaceous continental magmatic arc in southwestern Montana, consists of volcaniclastic strata and basaltic andesite lava flows. An intrusive complex represents the volcano's solidified magma chamber. Compositional diversity within components of the volcano appears to reflect evolution via about 50 percent fractional crystallization involving clinopyroxene and plagioclase. 40Ar/39Ar indicate that the volcano was active about 78?1 Ma.
Suggested Citation
Du Bray, E., Harlan, S.S., 1998, Geology, age, and tectonic setting of the Cretaceous Sliderock Mountain Volcano, Montana: U.S. Geological Survey Professional Paper 1602, 19 p., https://doi.org/10.3133/pp1602.
ISSN: 2330-7102 (online)
Publication type
Report
Publication Subtype
USGS Numbered Series
Title
Geology, age, and tectonic setting of the Cretaceous Sliderock Mountain Volcano, Montana
Series title
Professional Paper
Series number
1602
DOI
10.3133/pp1602
Year Published
1998
Language
ENGLISH
Publisher
U.S. Dept. of the Interior, U.S. Geological Survey ;
For sale by U.S. Geological Survey, Information Services,