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October 01, 1980
The occurrence and chemistry of epidote-clinozoisites in mafic gneisses from the Ruby Range, southwestern Montana
P. S. Dahl
;
P. S. Dahl
Kent State Univ., Dep. Geol., Kent, Ohio, United States
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L. M. Friberg
L. M. Friberg
Univ. Akron, Dep. Geol., Akron, Ohio, United States
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Rocky Mountain Geology (1980) 18 (2): 77–82.
Article history
first online:
03 Mar 2017
Citation
P. S. Dahl, L. M. Friberg; The occurrence and chemistry of epidote-clinozoisites in mafic gneisses from the Ruby Range, southwestern Montana. Rocky Mountain Geology 1980;; 18 (2): 77–82. doi:
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Index Terms/Descriptors
- Beaverhead County Montana
- clinozoisite
- epidote
- epidote group
- gneisses
- high-grade metamorphism
- Madison County Montana
- metamorphic rocks
- metamorphism
- mineral assemblages
- Montana
- orthosilicates
- petrology
- Precambrian
- retrograde metamorphism
- Ruby Mountains
- silicates
- sorosilicates
- temperature
- United States
- zoning
- Beartooth Orogeny
- southwest Montana
Latitude & Longitude
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