Petrology and phase equilibrium modeling of sapphirine + quartz assemblage from the Napier Complex, East Antarctica: Diagnostic evidence for Neoarchean ultrahigh-temperature metamorphism

Geoscience Frontiers

Volumn 4, Issue 6, 2013, Pages 655-666

  Shimizu, Hisako ^a   Tsunogae, Toshiaki ^a,b   Santosh, M ^c,d  

^a UNIVERSITY OF TSUKUBA   (Japan)

^b UNIVERSITY OF JOHANNESBURG   (South Africa)

^c CHINA UNIVERSITY OF GEOSCIENCES   (China)

^d KOCHI UNIVERSITY   (Japan)

Author keywords

Antarctica; Napier complex; Petrology; Pseudosection modeling; Ultrahigh temperature granulite

Indexed keywords

ARCHEAN; COLLISION ZONE; CRUSTAL STRUCTURE; GRANULITE FACIES; MODELING; OROGENY; P-T-T PATH; PETROLOGY; PHASE EQUILIBRIUM; QUARTZ; SAPPHIRINE; SUBDUCTION ZONE; TECTONIC EVOLUTION; ULTRAHIGH TEMPERATURE METAMORPHISM;

ANTARCTICA; EAST ANTARCTICA;

EID: 84887497585     PISSN: 16749871     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.gsf.2012.09.001     Document Type: Article

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