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PETROLOGY AND GEOCHEMISTRY OF THE TROMY GNEISS COMPLEX, SOUTH NORWAY, AN ALLEGED EXAMPLE OF PROTEROZOIC DEPLETED LOWER CONTINENTAL CRUST (1999)
A granulite-facies Precambrian meta-igneous gneiss complex at Tromy, South Norway, which was previously assumed to represent a fragment of strongly large ion lithophile element (LILE)-depleted lower continental crust, has been reinvestigated using major and trace element data, radiogenic isotopes and secondary ion mass spectrometry (SIMS) U-Pb geochronology.
Reference:
JOURNAL OF PETROLOGY VOLUME 40 NUMBER 6 PAGES 909-933, 1999
JOURNAL OF PETROLOGY VOLUME 40 NUMBER 6 PAGES 909-933, 1999
Organization:
MINERALOGICAL - GEOLOGICAL MUSEUM, SARS GATE 1, N-0562 OSLO, NORWAY
Norway
MINERALOGICAL - GEOLOGICAL MUSEUM, SARS GATE 1, N-0562 OSLO, NORWAY
Norway
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