The geochemistry and isotopic age of eclogites from the Belomorian Belt (Kola Peninsula): Evidence for subducted Archean oceanic crust

Russian Geology and Geophysics

Volumn 53, Issue 3, 2012, Pages 262-280

  Shchipansky, A A ^a   Khodorevskaya, L I ^b   Slabunov, A I ^c  

^a GEOLOGICAL INSTITUTE   (Russian Federation)

^b INSTITUTE OF EXPERIMENTAL MINERALOGY   (Russian Federation)

^c INSTITUTE OF GEOLOGY   (Russian Federation)

Author keywords

Archean; Eclogites; Isotope dating; Megam lange belt; Oceanic crust; Oceanic zircon; SHRIMP; Subduction; TTG gneisses

Indexed keywords

ARCHEAN; CRUSTAL CONTAMINATION; ECLOGITE; GEOCHEMISTRY; GNEISS; HIGH PRESSURE; ISOTOPIC COMPOSITION; MANTLE SOURCE; OCEANIC CRUST; PROTOLITH; PROVENANCE; SHRIMP DATING; SUBDUCTION ZONE; ZIRCON;

KOLA PENINSULA; MURMANSK [RUSSIAN FEDERATION]; RUSSIAN FEDERATION;

DECAPODA (CRUSTACEA);

EID: 84857309693     PISSN: 10687971     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.rgg.2012.02.004     Document Type: Article

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