Stability limits of hydrous minerals in sediment and mid-ocean ridge basalt compositions : Implications for water transport in subduction zones
- Author
- ONO, S1
[1] Geological Institute, University of Tokyo, Tokyo, Japan - Source
Journal of geophysical research. 1998, Vol 103, Num B8, pp 18253-18267 ; ref : 50 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)
- Association minérale Composition chimique Etude expérimentale Haute pression Haute température MORB Manteau sup Pélite Subduction Teneur eau Zone transition Basalte tholéïtique Basalte Roche clastique Roche ignée Roche sédimentaire Roche volcanique
- Keyword (en)
- mineral assemblages Chemical composition Experimental study High pressure High temperature Mid Ocean Ridge Basalt upper mantle pelite Subduction Water content transition zones tholeiitic basalt basalts clastic rocks igneous rocks sedimentary rocks volcanic rocks
- Keyword (es)
- Asociación mineral Composición química Estudio experimental Alta presión Alta temperatura MORB Manto globo sup Pelita Subducción Dosis agua Zona transición Basalto Roca clástica Roca ignea Roca sedimentaria Roca volcánica
- Classification
- 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
- 2405240
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
10.1029/98JB01351 
https://dx.doi.org/10.1029/98JB01351
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