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Magma genesis in subduction zones

Author
GILL, J
UCSC, dep. earth sci., Santa Cruz CA, United States
Conference title
29th international geological congress (Kyoto, 24 August - 3 September 1992)
Conference name
International geological congress (29 ; Kyoto 1992-08-24)
Source

29th international geological congress (Kyoto, 24 August - 3 September 1992). 1992 ; 2Vol ; p. 7

Scientific domain
Geology; Geophysics
Document type
Conference Paper
Language
English
Keyword (fr)
Analyse élément trace Arc volcanique Basalte Croûte terrestre Dynamique fluide Genèse Géochimie isotopique MORB Magmatisme Manteau sup OIB Répartition élément Variation spatiale Variation temporelle Zone subtropicale Roche ignée Roche volcanique
Keyword (en)
trace elements volcanic arcs basalts crust fluid dynamics genesis isotope geochemistry Mid Ocean Ridge Basalt igneous activity upper mantle Oceanic Island Basalt partitioning spatial variations time variations subtropical environment igneous rocks volcanic rocks
Keyword (es)
Análisis elementos traza Basalto Corteza terrestre Dinámica fluido Génesis Geoquímica isotópica MORB Magmatismo Manto globo sup OIB Repartición fase Variación espacial Variación temporal Zona subtropical Roca ignea Roca volcánica
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01F Crystalline rocks / 001E01F01 Igneous and metamorphic rocks petrology, volcanic processes, magmas

Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01L Tectonics. Structural geology. Plate tectonics

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
4021427

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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