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Grain boundary wetness of texturally equilibrated rocks, with implications for seismic properties of the upper mantle

Author
YOSHINO, Takashi1 ; TAKEI, Yasuko2 ; WARK, David A1 ; WATSON, E. Bruce1
[1] Department of Earth and Environmental Sciences, Rensselaer Polytechnic Institute, Troy, New York, United States
[2] Earthquake Research Institute, University of Tokyo, Tokyo, Japan
Source

Journal of geophysical research. 2005, Vol 110, Num B8, pp B08205.1-B08205.16 ; ref : 45 ref

ISSN
0148-0227
Scientific domain
Astronomy earth cosmic environment; Geology; Geophysics; Climatology, meteorology; Oceanography
Publisher
American Geophysical Union, Washington, DC
Publication country
United States
Document type
Article
Language
English
Keyword (fr)
Arrangement particule Basalte olivine Granulat Géométrie Joint grain Lherzolite Manteau sup Matière fondue Modèle Onde sismique Prévision Rapport aspect Sphéroïde aplati Vitesse onde Basalte Péridotite Roche ignée Roche plutonique Roche ultramafique Roche volcanique
Keyword (en)
packing olivine basalt aggregate geometry grain boundaries lherzolite upper mantle melts models seismic waves prediction Aspect ratio Oblate spheroid Wave velocity basalts peridotites igneous rocks plutonic rocks ultramafics volcanic rocks
Keyword (es)
Agregado Geometría Limite grano Lherzolita Manto globo sup Producto fundido Modelo Onda sísmica Previsión Relación dimensional Esferoide achatado Velocidad onda Basalto Peridotitis Roca ignea Roca granuda Roca volcánica
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
17118182

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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