High-temperature granite magmatism, crust-mantle interaction and the mesoproterozoic intracontinental evolution of the Musgrave Province, Central Australia

Journal of Petrology

Volumn 52, Issue 5, 2011, Pages 931-958

  Smithies, R H ^a   Howard, H M ^a   Evins, P M ^a   Kirkland, C L ^a   Kelsey, D E ^b   Hand, M ^b   Wingate, M T D ^a   Collins, A S ^b   Belousova, E ^c  

^a GEOLOGICAL SURVEY OF WESTERN AUSTRALIA   (Australia)

^b UNIVERSITY OF ADELAIDE   (Australia)

^c MACQUARIE UNIVERSITY   (Australia)

Author keywords

Charnockite; Granite geochemistry; Intracontinental magmatism; Mesoproterozoic; UHT conditions

Indexed keywords

CHARNOCKITE; CRUST-MANTLE BOUNDARY; CRUSTAL EVOLUTION; CRUSTAL THICKNESS; EMPLACEMENT; HIGH TEMPERATURE; IGNEOUS GEOCHEMISTRY; IGNEOUS INTRUSION; MAGMATISM; OROGENY; OUTCROP; PROTEROZOIC;

AUSTRALIA; MUSGRAVE RANGES;

EID: 79955410002     PISSN: 00223530     EISSN: 14602415     Source Type: Journal    
DOI: 10.1093/petrology/egr010     Document Type: Article

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