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Research Article|
December 01, 1997
Origin of sulfide blebs in variably metasomatized mantle xenoliths, Quaternary West Eifel volcanic field, Germany Available to Purchase
C. S. J. Shaw
C. S. J. Shaw
University of Western Ontario, Department of Earth Sciences, London, ON, Canada
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C. S. J. Shaw
University of Western Ontario, Department of Earth Sciences, London, ON, Canada
Publisher: Mineralogical Association of Canada
First Online:
02 Mar 2017
Online ISSN: 1499-1276
Print ISSN: 0008-4476
© 1997 Mineralogical Association of Canada
Mineralogical Association of Canada
The Canadian Mineralogist (1997) 35 (6): 1453–1463.
Article history
First Online:
02 Mar 2017
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CitationC. S. J. Shaw; Origin of sulfide blebs in variably metasomatized mantle xenoliths, Quaternary West Eifel volcanic field, Germany. The Canadian Mineralogist 1997;; 35 (6): 1453–1463. doi:
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Index Terms/Descriptors
- augite
- Cenozoic
- Central Europe
- chain silicates
- clinopyroxene
- Eifel
- Europe
- Germany
- igneous rocks
- inclusions
- mantle
- metasomatism
- mineral assemblages
- mineral composition
- partial melting
- peridotites
- petrography
- plutonic rocks
- provenance
- pyroxene group
- Quaternary
- Rhenish Schiefergebirge
- Rhineland-Palatinate Germany
- silicates
- sulfides
- ultramafics
- volcanic fields
- xenoliths
Latitude & Longitude
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