Polyphase formation and exhumation of high- to ultrahigh-pressure rocks in continental subduction zone: Numerical modeling and application to the Sulu ultrahigh-pressure terrane in eastern China
- Author
- ZHONGHAI LI1 2 ; GERYA, Taras V2 3
[1] Department of Earth Sciences, Nanjing University, Nanjing, China
[2] Geophysical Fluid Dynamics, Institute of Geophysics, Department of Earth Sciences, ETH-Zurich, Zurich, Switzerland
[3] Geology Department, Moscow State University, Moscow, Russian Federation - Source
Journal of geophysical research. 2009, Vol 114, Num B9 ; B09406.1-B09406.27 ; ref : 1 p.1/4
- 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
- Russian
- Keyword (fr)
- Age Chenal Croûte continentale Dalle Etude expérimentale Exhumation Extrusion Foyer Haute température Lithosphère Manteau Modèle numérique Modèle référence Panache Placage sous-crustal Plaque épaisse Pression Profondeur Roche métamorphique Simulation numérique Subduction Terrane Unité tectonique Zone subduction Chine Est Asie Chine Extrême Orient
- Keyword (en)
- age channels continental crust slabs experimental studies exhumation extrusions focus high temperature lithosphere mantle numerical models Reference model plumes underplating Thick plate pressure depth metamorphic rocks digital simulation subduction Terranes tectonic units subduction zones Eastern China Asia China Far East
- Keyword (es)
- Edad Canal Corteza continental Losa Alta temperatura Litosfera Abrigo Modelo referencia Penacho Placa espesa Presión Profundidad Roca metamórfica Simulación numérica Subducción Terrane Unidad tectónica Zona subducto China Este Asia China Extremo Oriente
- Classification
- Discipline
- Earth sciences
- Origin
- Inist-CNRS
- Database
- PASCAL
- INIST identifier
- 22135662
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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