The high PT stability of apatite and Cl partitioning between apatite and hydrous potassic phases in peridotite: An experimental study to 19 GPa with implications for the transport of P, Cl and K in the upper mantle

Contributions to Mineralogy and Petrology

Volumn 163, Issue 2, 2012, Pages 277-296

  Konzett, Jürgen ^a   Rhede, Dieter ^b   Frost, Daniel J ^c  

^a UNIVERSITY OF INNSBRUCK   (Austria)

^b GFZ GERMAN RESEARCH CENTRE FOR GEOSCIENCES   (Germany)

^c UNIVERSITÄT BAYREUTH   (Germany)

Author keywords

Apatite; Cl OH partitioning; High pressure; Peridotite

Indexed keywords

APATITE; CHLORINE; EXPERIMENTAL MINERALOGY; FLUID COMPOSITION; FLUID INCLUSION; HIGH PRESSURE; HIGH TEMPERATURE; PARTITIONING; PERIDOTITE; PHOSPHORUS; POTASSIC ROCK; POTASSIUM; TRACE ELEMENT; TRANSPORT PROCESS; UPPER MANTLE;

EID: 84856222503     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-011-0672-x     Document Type: Article

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