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Research Article|
September 01, 1990
Fluid-inclusions evidence for the physical and chemical conditions associated with intermediate-temperature PGE mineralization at the New Rambler Deposit, southeastern Wyoming
Matthew W. Nyman;
Matthew W. Nyman
Va. Polytech. Inst. and State Univ., Dep. Geol. Sci., Blacksburg, VA, United States
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The Canadian Mineralogist (1990) 28 (3): 629–638.
Article history
first online:
02 Mar 2017
Citation
Matthew W. Nyman, Ronald W. Sheets, Robert J. Bodnar; Fluid-inclusions evidence for the physical and chemical conditions associated with intermediate-temperature PGE mineralization at the New Rambler Deposit, southeastern Wyoming. The Canadian Mineralogist 1990;; 28 (3): 629–638. doi:
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Index Terms/Descriptors
- albite
- alteration
- calcium chloride
- carbon dioxide
- chemically precipitated rocks
- chlorite
- chlorite group
- clinozoisite
- copper ores
- economic geology
- epidote
- epidote group
- evaporites
- feldspar group
- fluid inclusions
- framework silicates
- geologic thermometry
- gold ores
- histograms
- inclusions
- magnetite
- Medicine Bow Mountains
- metal ores
- metasomatism
- mineral deposits, genesis
- nitrogen
- North America
- ore minerals
- ore-forming fluids
- orthosilicates
- oxides
- paleosalinity
- paragenesis
- petrography
- petrology
- plagioclase
- platinum ores
- polymetallic ores
- processes
- remobilization
- Rocky Mountains
- salt
- sedimentary rocks
- sheet silicates
- silicates
- sorosilicates
- statistical analysis
- U. S. Rocky Mountains
- United States
- wall-rock alteration
- water
- Wyoming
- southeastern Wyoming
- New Rambler Deposit
Latitude & Longitude
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