Relative impact of mantle densification and eclogitization of slabs on subduction dynamics: A numerical thermodynamic/thermokinematic investigation of metamorphic density evolution

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Understanding the relationships between density and spatio-thermal variations at convergent plate boundaries is important for deciphering the present-day dynamics and evolution of subduction zones. In particular, the interaction between densification due to mineralogical phase transitions and slab p...

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Autor principal: Duesterhoeft, E.
Otros Autores: Quinteros, J., Oberhänsli, R., Bousquet, R., de Capitani, C.
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: Elsevier 2014
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100 1 |a Duesterhoeft, E. 
245 1 0 |a Relative impact of mantle densification and eclogitization of slabs on subduction dynamics: A numerical thermodynamic/thermokinematic investigation of metamorphic density evolution 
260 |b Elsevier  |c 2014 
270 1 0 |m Duesterhoeft, E.; Institute of Geosciences, University of Kiel, Ludewig-Meyn-Str. 10, Germany 
506 |2 openaire  |e Política editorial 
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520 3 |a Understanding the relationships between density and spatio-thermal variations at convergent plate boundaries is important for deciphering the present-day dynamics and evolution of subduction zones. In particular, the interaction between densification due to mineralogical phase transitions and slab pull forces is subject to ongoing investigations. We have developed a two-dimensional subduction zone model that is based on thermodynamic equilibrium assemblage calculations and includes the effects of melting processes on the density distribution in the lithosphere. Our model calculates the "metamorphic density" of rocks as a function of pressure, temperature and chemical composition in a subduction zone down to 250. km. We have used this model to show how the hydration, dehydration, partial melting and fractionation processes of rocks all influence the metamorphic density and greatly depend on the temperature field within the subduction system. These processes are largely neglected by other approaches that reproduce the density distribution within this complex tectonic setting. Our model demonstrates that the initiation of eclogitization (i.e., when crustal rocks reach higher densities than the ambient mantle) of the slab is not the only significant process that makes the descending slab denser and generates the slab pull force. Instead, the densification of the lithospheric mantle of the sinking slab starts earlier than eclogitization and contributes significantly to slab pull in the early stages of subduction. Accordingly, the complex metamorphic structure of the slab and the mantle wedge has an important impact on the development of subduction zones. © 2014 Elsevier B.V.  |l eng 
536 |a Detalles de la financiación: State University of New York Potsdam 
536 |a Detalles de la financiación: Deutsche Forschungsgemeinschaft, SPP 1257 
536 |a Detalles de la financiación: Deutsche Forschungsgemeinschaft 
536 |a Detalles de la financiación: The research was supported by DFG research grant SPP 1257 project 6.2 and the Graduate School GRK1364 Shaping Earth's Surface in a Variable Environment funded by the German Research Foundation (DFG), co-financed by the federal state of Brandenburg and the University of Potsdam. We thank Olivier Vanderhaeghe and an anonymous colleague for their positive reviews, which helped to improve the quality of this manuscript. Appendix A 
593 |a Institute of Earth and Environmental Science, University of Potsdam, Karl-Liebknecht-Str. 24-25, Potsdam-Golm, 14476, Germany 
593 |a Institute of Geosciences, University of Kiel, Ludewig-Meyn-Str. 10, Kiel, 24118, Germany 
593 |a Deutsches GeoForschungsZentrum GFZ, Telegrafenberg, Potsdam, 14473, Germany 
593 |a Department of Computer Sciences, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Buenos Aires, C1428EGA, Argentina 
593 |a Institute of Mineralogy and Petrography, University of Basel, Bernoullistrasse 30, Basel, 4056, Switzerland 
690 1 0 |a DENSITY 
690 1 0 |a MELT 
690 1 0 |a METAMORPHISM 
690 1 0 |a SUBDUCTION 
690 1 0 |a THERMO-MECHANICAL MODELING 
690 1 0 |a THERMODYNAMIC MODELING 
690 1 0 |a DENSIFICATION 
690 1 0 |a DENSIFICATION 
690 1 0 |a DENSITY (SPECIFIC GRAVITY) 
690 1 0 |a DENSITY (SPECIFIC GRAVITY) 
690 1 0 |a MELTING 
690 1 0 |a MELTING 
690 1 0 |a PHASE TRANSITIONS 
690 1 0 |a PHASE TRANSITIONS 
690 1 0 |a STRUCTURAL GEOLOGY 
690 1 0 |a STRUCTURAL GEOLOGY 
690 1 0 |a TECTONICS 
690 1 0 |a TECTONICS 
690 1 0 |a THERMODYNAMICS 
690 1 0 |a THERMODYNAMICS 
690 1 0 |a CONVERGENT PLATE BOUNDARIES 
690 1 0 |a CONVERGENT PLATE BOUNDARIES 
690 1 0 |a METAMORPHIC STRUCTURES 
690 1 0 |a METAMORPHIC STRUCTURES 
690 1 0 |a METAMORPHISM 
690 1 0 |a METAMORPHISM 
690 1 0 |a SUBDUCTION 
690 1 0 |a SUBDUCTION 
690 1 0 |a SUBDUCTION ZONE MODELING 
690 1 0 |a SUBDUCTION ZONE MODELING 
690 1 0 |a THERMODYNAMIC EQUILIBRIA 
690 1 0 |a THERMODYNAMIC EQUILIBRIA 
690 1 0 |a THERMODYNAMIC MODEL 
690 1 0 |a THERMODYNAMIC MODEL 
690 1 0 |a THERMOMECHANICAL MODEL 
690 1 0 |a THERMOMECHANICAL MODEL 
690 1 0 |a METAMORPHIC ROCKS 
690 1 0 |a MANTLE STRUCTURE 
690 1 0 |a METAMORPHISM 
690 1 0 |a PLATE BOUNDARY 
690 1 0 |a PLATE CONVERGENCE 
690 1 0 |a SLAB 
690 1 0 |a SUBDUCTION ZONE 
690 1 0 |a THERMODYNAMICS 
700 1 |a Quinteros, J. 
700 1 |a Oberhänsli, R. 
700 1 |a Bousquet, R. 
700 1 |a de Capitani, C. 
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