Sinossi
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.
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Contenuti
Preface; N. Bagdassarov, et al. List of Contributors. 1. Rheology of Partially Molten Rocks; D.L. Kohlstedt, et al. 2. Anelastic and Viscoelastic Behaviour of Partially Molten Rocks and Lavas; N. Bagdassarov. 3. Constraints on the Melt Distribution in Anisotropic Polycrystalline Aggregates Undergoing Grain Growth; U.H. Faul. 4. The Grain-Scale Distribution of Silicate, Carbonate and Metallosulfide Partial Melts: A Review of Theory and Experiments; D. Laporte, A. Provost. 5. Partial Melting and Melt Segregation in a Convecting Mantle; H. Schmeling. 6. A Fractionation Model for Hydrous Calcalkaline Plutons and the Heat Budget During Fractional Crystallisation and Assimilation; L. Matile, et al. 7. Migmatitic Gabbros from a Shallow-Level Metamorphic Contact Aureole, Fuerteventura Basal Complex, Canary Islands. Role of Deformation in Melt Segregation; A. Hobson, et al. 8. Thin Amorphous Intergranular Layers at Mineral Interfaces in Xenoliths: the Early Stage of Melting; R. Wirth, L. Franz. Index.
Product Description
Book by Laporte Didier Thompson Alan B
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Buch. Condizione: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -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. 292 pp. Englisch. Codice articolo 9780412847202
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Gebunden. Condizione: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. 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 o. Codice articolo 5915353
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Condizione: New. This text provides an 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. Editor(s): Bagdassarov, Nick; Laporte, D.; Thompson, Alan Bruce. Series: Petrology and Structural Geology. Num Pages: 287 pages, biography. BIC Classification: RBGG; RBGK. Category: (P) Professional & Vocational; (UP) Postgraduate, Research & Scholarly; (UU) Undergraduate. Dimension: 235 x 155 x 17. Weight in Grams: 586. . 1999. Hardback. . . . . Codice articolo V9780412847202
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Buch. Condizione: Neu. Physics and Chemistry of Partially Molten Rocks | N. Bagdassarov (u. a.) | Buch | xvi | Englisch | 1999 | Springer Netherland | EAN 9780412847202 | Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg, juergen[dot]hartmann[at]springer[dot]com | Anbieter: preigu Print on Demand. Codice articolo 102552576
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Buch. Condizione: Neu. This item is printed on demand - Print on Demand Titel. Neuware -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.Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg 292 pp. Englisch. Codice articolo 9780412847202
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Buch. Condizione: Neu. Druck auf Anfrage Neuware - Printed after ordering - 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. Codice articolo 9780412847202
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Condizione: New. This text provides an 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. Editor(s): Bagdassarov, Nick; Laporte, D.; Thompson, Alan Bruce. Series: Petrology and Structural Geology. Num Pages: 287 pages, biography. BIC Classification: RBGG; RBGK. Category: (P) Professional & Vocational; (UP) Postgraduate, Research & Scholarly; (UU) Undergraduate. Dimension: 235 x 155 x 17. Weight in Grams: 586. . 1999. Hardback. . . . . Books ship from the US and Ireland. Codice articolo V9780412847202
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