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Physics and Chemistry of Partially Molten Rocks

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Description

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.
Release date Australia
December 31st, 1999
Audiences
  • Postgraduate, Research & Scholarly
  • Professional & Vocational
  • Undergraduate
Contributors
  • Edited by Alan Bruce Thompson
  • Edited by D. Laporte
  • Edited by N. Bagdassarov
Illustrations
XVI, 271 p.
Pages
271
Dimensions
155x235x17
ISBN-13
9780412847202
Product ID
2436663

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