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Field measurement of slow metamorphic reaction rates at temperatures of 500° to 600°C

Author
BAXTER, E. F1 ; DEPAOLO, D. J1
[1] Department of Geology and Geophysics, University of California, 301 McCone Hall, Berkeley, CA 94720, United States
Source

Science (Washington, D.C.). 2000, Vol 288, Num 5470, pp 1411-1414 ; Illustration

CODEN
SCIEAS
ISSN
0036-8075
Scientific domain
Multidisciplinary
Publisher
American Association for the Advancement of Science, Washington, DC
Publication country
United States
Document type
Article
Language
English
Keyword (fr)
Condition pression température Grenat Haute température Interaction fluide roche Isotope Métamorphisme Refroidissement Roche totale Sr 87-Sr 86 Strontium Région Simplon Suisse Europe Nésosilicate Silicate Europe Centrale
Keyword (en)
P-T conditions garnet high temperature fluid-rock interaction isotopes metamorphism cooling whole rock Sr-87/Sr-86 strontium Simplon region Switzerland Europe nesosilicates silicates Central Europe
Keyword (es)
Condición PT Granate Alta temperatura Interacción flúido roca Isótopo Metamorfismo Enfriamiento Roca total Sr 87-Sr 86 Estroncio Región Simplon Suiza Europa Silicato Europa central
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01C Isotope geochemistry. Geochronology / 001E01C01 Isotope geochemistry

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

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
1429429

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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