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Friction falls towards zero in quartz rock as slip velocity approaches seismic rates

Author
DI TORO, Giulio1 ; GOLDSBY, David L2 ; TULLIS, Terry E2
[1] Dipartimento di Geologia, Paleontologia e Geofisica, Universita'di Padova, Padova, 35137, Italy
[2] Department of Geological Sciences, Brown University, Providence, Rhode Island 02912, United States
Source

Nature (London). 2004, Vol 427, Num 6973, pp 436-439, 4 p ; Illustration ; ref : 30 ref

CODEN
NATUAS
ISSN
0028-0836
Scientific domain
Multidisciplinary
Publisher
Nature Publishing, London
Publication country
United Kingdom
Document type
Article
Language
English
Keyword (fr)
Accélération Composition siliceuse Contrainte cisaillement Dommage catastrophe naturelle Déplacement faille Etude expérimentale Frottement Gel Glissement Magnitude Mécanisme Onde sismique Plan faille Quartz Silice Séisme Vitesse Résistance frottement Résistance glissement Silicate Tectosilicate
Keyword (en)
acceleration siliceous composition shear stress natural disaster damages fault displacements experimental studies friction gels slip magnitude mechanism seismic waves fault planes quartz silica earthquakes velocity silicates framework silicates
Keyword (es)
Composición silícea Tensión cizallamiento Daño catástrofe natural Desplazamiento falla Magnitud Onda sísmica Plano falla Cuarzo Sílice Sismo Velocidad Silicato
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01L Tectonics. Structural geology. Plate tectonics

Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01M Internal geophysics / 001E01M03 Earthquakes, seismology

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
16467000

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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