Geochemistry of high-temperature granulitic supracrustals from Rogaland, SW Norway
Publication date
1990-06-11
Authors
Bol, L.C.G.M.
Editors
Advisors
Supervisors
Schuiling, R.D.
Jansen, J.B.H.
DOI
Document Type
Dissertation
Metadata
Show full item recordCollections
License
Abstract
Were the granulite-facies metamorphic supracrustals of the Faurefjell Metasediment Formation in Rogaland, SW Norway, chemically open or closed systems? In order to assess differential element mobilities in response to pre-, syn- and post-metamorphic fluid fluxes through this formation, the mineralogy, crystal chemistry, bulk chemical composition, and mineral oxygen and carbon stable isotope composition is investigated in marbles and metavolcanics.
Keywords
granulite, geochemistry, Rogaland fylke, Norway, metamorphic petrology, stable isotopes
Citation
Bol, L C G M 1990, 'Geochemistry of high-temperature granulitic supracrustals from Rogaland, SW Norway', Doctor of Philosophy, Universiteit Utrecht, Utrecht.