Fluorine in nominally fluorine-free mantle minerals: Experimental partitioning of F between olivine, orthopyroxene and silicate melts with implications for magmatic processes

Earth and Planetary Science Letters

Volumn 337-338, Issue , 2012, Pages 1-9

  Beyer, C ^a   Klemme, S ^a   Wiedenbeck, M ^b   Stracke, A ^a   Vollmer, C ^a  

^a UNIVERSITY OF MÜNSTER   (Germany)

^b GFZ GERMAN RESEARCH CENTRE FOR GEOSCIENCES   (Germany)

Author keywords

Chlorine; Fluorine; Mantle; Olivine; Partition coefficient; Peridotite

Indexed keywords

BASALTIC MELTS; DEPLETED MORB MANTLES; EARTH'S MANTLE; FLUORINE CONTENT; FLUORINE-FREE; HALOGEN-FREE; HIGH-RESOLUTION TEM; MAGMATIC PROCESS; MANTLE; MANTLE MINERALS; MANTLE SOURCE; MELT INCLUSIONS; MID-OCEAN RIDGE BASALT; NATURAL COMPOSITION; OCEAN ISLAND BASALTS; OCEANIC BASALTS; OLIVINE STRUCTURES; ORTHOPYROXENE; OXYGEN DEFECT; PARTITION COEFFICIENT; PERIDOTITE; SILICATE MELTS; SPINEL PERIDOTITES; UPPER MANTLE;

BASALT; CHLORINE; HYDROGEN; IGNEOUS ROCKS; MINERALS; OLIVINE; SILICATES; SODIUM; STRUCTURAL GEOLOGY;

FLUORINE;

CHEMICAL COMPOSITION; CHLORINE; EXPERIMENTAL MINERALOGY; FLUORINE; MAGMATISM; MANTLE; MELT INCLUSION; MID-OCEAN RIDGE BASALT; OLIVINE; ORTHOPYROXENE; PARTITION COEFFICIENT; PERIDOTITE; PRESSURE; SILICATE MELT; TEMPERATURE;

EID: 84862338075     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2012.05.003     Document Type: Article

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