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 different...

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Weitere Verfasser:	Bagdassarov, Nick (HerausgeberIn), Laporte, Didier (HerausgeberIn), Thompson, Alan Bruce (HerausgeberIn)
Format:	Elektronisch E-Book
Sprache:	English
Veröffentlicht:	Dordrecht Springer Netherlands 2000
Schriftenreihe:	Petrology and Structural Geology 11
Schlagworte:	Earth Sciences Mineralogy Geophysics/Geodesy Earth sciences Geophysics Schmelze Mantelgestein Erdmantel Silicatschmelze Konferenzschrift > 1997 > Straßburg
Online-Zugang:	BTU01 Volltext
Zusammenfassung:	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
Beschreibung:	1 Online-Ressource (XVI, 271 p)
ISBN:	9789401140164
DOI:	10.1007/978-94-011-4016-4