Geochemical systematics of komatiite-tholeiite and adakitic-arc basalt associations: The role of a mantle plume and convergent margin in formation of the Sandur Superterrane, Dharwar craton, India

Lithos

Volumn 106, Issue 1-2, 2008, Pages 155-172

  Manikyamba, C ^a   Kerrich, R ^b   Khanna, T C ^a   Keshav Krishna, A ^a   Satyanarayanan, M ^a  

^a NATIONAL GEOPHYSICAL RESEARCH INSTITUTE   (India)

^b UNIVERSITY OF SASKATCHEWAN   (Canada)

Author keywords

Adakites; Arcs; Komatiites; Plumes; Sandur Superterrane; Terrane accretion

Indexed keywords

ADAKITE; CONVERGENT MARGIN; DEFORMATION; FRACTIONAL CRYSTALLIZATION; IGNEOUS GEOCHEMISTRY; ISOTOPIC RATIO; KOMATIITE; MANTLE PLUME; METAMORPHISM; OCEAN ISLAND BASALT; OLIVINE; TEXTURE; THOLEIITIC BASALT;

ASIA; DHARWAR CRATON; EURASIA; INDIA; KARNATAKA; SANDUR BELT; SOUTH ASIA;

SPINIFEX;

EID: 54449088403     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2008.07.003     Document Type: Article

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