Multiple generations of granite in the Fosdick Mountains, Marie Byrd Land, West Antarctica: Implications for polyphase intracrustal differentiation in a continental margin setting

Journal of Petrology

Volumn 51, Issue 3, 2010, Pages 627-670

  Korhonen, F J ^a   Saito, S ^a,b   Brown, M ^a   Siddoway, C S ^c   Day, J M D ^a  

^a University of Maryland   (United States)

^b JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

^c Department of Psychology   (United States)

Author keywords

Active continental margin; Anatexis; Antarctica; Crustal differentiation; East Gondwana; Fosdick Mountains; Granite petrogenesis; Migmatite

Indexed keywords

ANATEXIS; CALC ALKALINE ROCK; DIKE; DISSOLUTION; EMPLACEMENT; EXHUMATION; GRANITE; GRANODIORITE; ISOTOPIC COMPOSITION; MIGMATITE; PARTIAL MELTING; PETROGENESIS; PLUTON; SILL; SOURCE ROCK; TRACE ELEMENT; TURBIDITE;

ANTARCTICA; MARIE BYRD LAND; WEST ANTARCTICA;

EID: 77749279555     PISSN: 00223530     EISSN: 14602415     Source Type: Journal    
DOI: 10.1093/petrology/egp093     Document Type: Article

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