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Physics and chemistry of partially molten rocks [Libro electrónico] / editors: Nick Bagdassarov, Didier Laporte, Alan Bruce Thompson

Bagdassarov, Nick [editor] | Laporte, Didier [editor/a] | Thompson, Alan Bruce [editor/a].
Tipo de material: Libro en línea Libro en línea Editor: Dordrecht: Springer science, c2000Descripción: xvi, 271 páginas : fotografías, gráf., ilustraciones ; centímetros.ISBN: 9401057745; 9789401057745; 9789401140164 (Online).Nota de acceso: Disponible para usuarios de ECOSUR con su clave de acceso Nota de bibliografía: Incluye bibliografía e índice: páginas 269-271 Número de sistema: 57170Resumen:
Inglés

Partial melting occurs in a variety of geological environments, from granitic partial melts in the continental crust, to basaltic or carbonate partial melts in the upper mantle. Partial melting is the first stage of magmatism and therefore plays a role of primary importance in the chemical differentiation of the Earth and in the transport of heat to the Earth surface. This special volume contains contributions presented at the symposium Physics and Chemistry of Partially Molten Systems' of the EUG 9 meeting, held in Strasbourg, France, on March 23-27, 1997. It is intended to provide a current understanding of the physics of partial melting and melt segregation and covers topics such as the rheology of partially molten systems, the topology of partial melts, modelling of partial melting processes, and field observations of partial melts. Audience: This book is intended for a broad readership, including graduate students, specializing in petrology and geodynamics. The volume may be recommended as a textbook for graduate courses on petrology, geomaterial sciences and geophysics.

Recurso en línea: http://link.springer.com/book/10.1007%2F978-94-011-4016-4
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Incluye bibliografía e índice: páginas 269-271

Disponible para usuarios de ECOSUR con su clave de acceso

Partial melting occurs in a variety of geological environments, from granitic partial melts in the continental crust, to basaltic or carbonate partial melts in the upper mantle. Partial melting is the first stage of magmatism and therefore plays a role of primary importance in the chemical differentiation of the Earth and in the transport of heat to the Earth surface. This special volume contains contributions presented at the symposium Physics and Chemistry of Partially Molten Systems' of the EUG 9 meeting, held in Strasbourg, France, on March 23-27, 1997. It is intended to provide a current understanding of the physics of partial melting and melt segregation and covers topics such as the rheology of partially molten systems, the topology of partial melts, modelling of partial melting processes, and field observations of partial melts. Audience: This book is intended for a broad readership, including graduate students, specializing in petrology and geodynamics. The volume may be recommended as a textbook for graduate courses on petrology, geomaterial sciences and geophysics. eng

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