Cr-spinel, an excellent micro-container for retaining primitive melts - Implications for a hydrous plume origin for komatiites

Earth and Planetary Science Letters

Volumn 189, Issue 3-4, 2001, Pages 177-188

  Shimizu, Kenji ^a   Komiya, Tsuyoshi ^a   Hirose, Kei ^a   Shimizu, Nobumichi ^b   Maruyama, Shigenori ^a  

^a TOKYO INSTITUTE OF TECHNOLOGY   (Japan)

^b WOODS HOLE OCEANOGRAPHIC INSTITUTION   (United States)

Author keywords

Belingwe greenstone belt; Chrome spinel; High pressure; Inclusions; Komatiite; Plumes; Transition zones

Indexed keywords

CHROME SPINEL; GREENSTONE BELT; KOMATIITE; MANTLE PLUME; PETROLOGY; SPINEL;

ZIMBABWE;

EID: 0034907874     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0012-821X(01)00359-4     Document Type: Article

References (40)

1. Water and sulfur contents of melt inclusions from Archean komatiites
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3. Melting of peridotite to 14 GPa and the genesis of komatiites
4. Melting experiments on anhydrous peridotite KLB-1: Compositions of magmas in the upper mantle and transition zone
5. Constraining the potential temperature of the Archaean mantle a review of the evidence from komatiites
6. High pressure melting of pyrolite under hydrous condition and its geophysical implication
7. 2O-saturated mantle peridotite to 11 gigapascals
8. Evidence for hydrous high-MgO melts in the Precambrian
9. Emplacement conditions of komatiite magmas from the 3.49 Ga Komati Formation, Barberton Greenstone Belt, South Africa
10. Were komatiites wet?
11. Uniquely fresh 2.7 Ga komatiites from the Belingwe greenstone belt, Zimbabwe
12. 2O-bearing Phanerozoic ultramafic melt inclusions in phenocrysts from Papua-New Guinea Boninite
13. Methodology for the study of melt inclusions in Cr-spinel, and implications for parental melts of MORB from FAMOUS area
14. Primitive basaltic melts included in podiform chromites from the Oman ophiolite
15. Quantitative analysis of rock samples by an X-ray fluorescence spectrometer (I)
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38. 4: A new water reservoir in lower-most upper mantle
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40. 4