Trace element partitioning during high-P partial melting and melt-rock interaction; an example from northern Fiordland, New Zealand

Journal of Metamorphic Geology

Volumn 22, Issue 5, 2004, Pages 443-457

  Schroter F C ^a   Stevenson, J A ^a   Daczko, N R ^a,b   Clarke, G L ^a   Pearson, N J ^b   Klepeis, K A ^c  

^a UNIVERSITY OF SYDNEY   (Australia)

^b MACQUARIE UNIVERSITY   (Australia)

^c UNIVERSITY OF VERMONT   (United States)

Author keywords

Garnet granulite; Laser Ablation Inductively Coupled Plasma Mass Spectrometer; Partial melting; Trace and REE; Two pyroxene hornblende granulite

Indexed keywords

GRANULITE FACIES; HIGH PRESSURE; METAMORPHISM; PARTIAL MELTING; PARTITIONING; TRACE ELEMENT;

AUSTRALASIA; FIORDLAND NATIONAL PARK; NEW ZEALAND; SOUTH ISLAND; SOUTHLAND;

EID: 3242883248     PISSN: 02634929     EISSN: None     Source Type: Journal    
DOI: 10.1111/j.1525-1314.2004.00525.x     Document Type: Article

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