W isotope compositions of oceanic islands basalts from French Polynesia and their meaning for core-mantle interaction

Chemical Geology

Volumn 260, Issue 1-2, 2009, Pages 37-46

  Takamasa, Asako ^a   Nakai, Shun'ichi ^a   Sahoo, YuVin ^a   Hanyu, Takeshi ^b   Tatsumi, Yoshiyuki ^b  

^a UNIVERSITY OF TOKYO   (Japan)

^b JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

Author keywords

Core mantle interaction; Hf W; HIMU ocean island basalts; Mantle isotope systematics

Indexed keywords

CLINOPYROXENE; CORE-MANTLE BOUNDARY; FRACTIONATION; ISOTOPIC COMPOSITION; MAGMATIC DIFFERENTIATION; MANTLE CHEMISTRY; MANTLE SOURCE; MELTING; OCEAN ISLAND BASALT; OLIVINE; SEISMIC TOMOGRAPHY; TUNGSTEN; UPWELLING;

AUSTRAL ISLANDS; COOK ISLANDS; FRENCH POLYNESIA; MANGAIA; PACIFIC ISLANDS; PACIFIC OCEAN; POLYNESIA; RAROTONGA; RURUTU; TUBUAI;

EID: 60249090598     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.chemgeo.2008.11.018     Document Type: Article

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