Majorite fractionation and genesis of komatiites in the deep mantle
- Other title
- Fractionnement de Majorite et genèse de komatïtes dans les zones profondes du manteau (fr)
- Author
- OHTANI, E
Tohoku univ., inst. mineralogy petrology economic geology, Sendai 980, Japan - Conference name
- Early developments of the earth and Archaean geochemistry. Symposium (Paris 1988-08-29)
- Source
Precambrian research. 1990, Vol 48, Num 3, pp 195-202, 8 p ; Illustration , Table ; ref : 26 ref
- Publisher
- Elsevier, Amsterdam
- Publication country
- Netherlands
- Document type
- Conference Paper
- Language
- English
- Keyword (fr)
- Accrétion Archéen Ceinture roche verte Coefficient partage Convection Cristallisation fractionnée Diagramme équilibre Elément lithophile Expérience Fractionnement chimique Fusion Groupe grenat Hétérogénéité Komatiite Majorite Manteau sup Modèle Manteau appauvri Manteau primitif Pétrogenèse Zone transition Antécambrien
- Keyword (en)
- Accretion Archean Greenstone belts Partition coefficient Partition coefficients Convection Fractional crystallization Phase equilibria Lithophile elements Experience Experimental studies Chemical fractionation Melting Orthosilicates, garnet group Heterogeneity Komatiite Majorite Upper mantle Models Precambrian
- Keyword (es)
- Acreción Arqueano Cinturón ofiolítico Coeficiente repartición Convección Cristalización fraccionada Diagrama equilibrio Elemento litófilo Experiencia Fraccionamiento químico Fusión Grupo granate Heterogeneidad Majorita Manto globo sup Modelo Antecámbrico
- Classification
- Pascal
- 001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01A Mineralogy / 001E01A02 Silicates
- Pascal
- 001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01F Crystalline rocks / 001E01F02 Experimental petrology
- Discipline
- Earth sciences
- Origin
- Inist-CNRS
- Database
- PASCAL
- INIST identifier
- 19403935
Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS
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DOI
10.1016/0301-9268(90)90008-E 
https://dx.doi.org/10.1016/0301-9268(90)90008-E
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