Physics and Chemistry of Partially Molten Rocks
Published on 31. December 1999
Book
Hardback
XVI, 271 pages
978-0-412-84720-2 (ISBN)
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.
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.
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.
More details
Series
Edition
2000 ed.
Language
English
Place of publication
Dordrecht
Netherlands
Target group
College/higher education
Professional and scholarly
Research
Illustrations
XVI, 271 p.
Dimensions
Height: 241 mm
Width: 160 mm
Thickness: 21 mm
Weight
606 gr
ISBN-13
978-0-412-84720-2 (9780412847202)
DOI
10.1007/978-94-011-4016-4
Schweitzer Classification
Other editions
Additional editions
N. Bagdassarov | D. Laporte | Alan Bruce Thompson
Physics and Chemistry of Partially Molten Rocks
E-Book
12/2012
Springer
€96.29
Available for download
N. Bagdassarov | D. Laporte | Alan Bruce Thompson
Physics and Chemistry of Partially Molten Rocks
Book
09/2012
Springer
€106.99
Shipment within 15-20 days
Content
1. Rheology of Partially Molten Rocks.- 1. Introduction.- 2. Constitutive equations.- 3. Discussion.- 2. Anelastic and Viscoelastic Behaviour of Partially Molten Rocks and Lavas.- 1. Introduction.- 2. Experimental methods of Q measurement.- 3. Experiments.- 4. Discussion.- 5. Conclusions.- 3. Constraints on the Melt Distribution in Anisotropic Polycrystalline Aggregates Undergoing Grain Growth.- 1. Introduction.- 2. Surface energy considerations.- 3. Experimental observations: the system olivine + basaltic melt.- 4. Summary and implications for partial melts in the mantle.- 4. The Grain-scale Distribution of Silicate, Carbonate and Metallosulfide Partial Melts: a Review of Theory and Experiments.- 1. Introduction.- 2. Interfacial energies.- 3. Textural equilibrium.- 4. Equilibrium melt distribution in an idealized partially molten system.- 5. Wetting properties of geological partial melts.- 6. Discussion.- 5. Partial Melting and Melt Segregation in a Convecting Mantle.- 1. Introduction.- 2. General aspects of melting in the mantle.- 3. The physics of melt generation, segregation and convection.- 4. Case studies relevant for melting and segregation in a convecting mantle.- 5. Conclusions.- 6. A Fractionation Model for Hydrous Calc-Alkaline Plutons and the Heat Budget During Fractional Crystallisation and Assimilation.- 1. Introduction.- 2. Fractional crystallisation of hydrous mantle magma.- 3. Crystallisation(C), fractional crystallisation (FC) and assimilation (A) hydrous mantle magmas.- 4. Comparison of the heat balance for AFC processes with other results for crustal melting.- 5. Conclusions.- 7. Migmaticic Gabbros From a Shallow-Level Metamorphic Contact Aureole, Fuerteventura Basal Complex, Canary Islands: Role of Deformation in Melt Segregation.- 1. Introduction.-2. Tectonic and geological setting.- 3. The PX1 intrusion and its host rock.- 4. Partial melting and mechanisms of melt segregation.- 5. Rheology of partly molten rocks.- 6. Discussion.- 7. Conclusion.- 8. Thin Amorphous Intergranular Layers at Mineral Interfaces in Xenoliths: the Early Stage of Melting.- 1. Introduction.- 2. Sample preparation and analytical methods.- 3. Sample description.- 4. Definitions.- 5. Results.- 6. Discussion.