Metasomatism and the Chemical Transformation of Rock: The Role of Fluids in Terrestrial and Extraterrestrial Processes - Couverture souple

Livre 4 sur 14: Lecture Notes in Earth System Sciences

Harlov, Daniel ; Austrheim, Hakon

9783662520642: Metasomatism and the Chemical Transformation of Rock: The Role of Fluids in Terrestrial and Extraterrestrial Processes

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ISBN 10 : 3662520648 ISBN 13 : 9783662520642

Editeur : Springer-Verlag Berlin and Heidelberg GmbH & Co. K, 2016

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This book examines how metasomatism influences and helps to control both the evolution and stability of the crust and lithospheric mantle.

Les informations fournies dans la section � Synopsis � peuvent faire r�f�rence � une autre �dition de ce titre.

� propos de l?auteur

Prof. Dr. Daniel E. Harlov, GeoForschungsZentrum Potsdam, Germany - dharlov@gfz-potsdam.de Prof. Dr. H�kon Austrheim, University of Oslo, Norway h.o.austrheim@geo.uio.no

Les informations fournies dans la section � A propos du livre � peuvent faire r�f�rence � une autre �dition de ce titre.

�diteur: Springer-Verlag Berlin and Heidelberg GmbH & Co. K
Date d'�dition: 2016
Langue: anglais
ISBN 10: 3662520648
ISBN 13: 9783662520642
Reliure: Broch�
Nombre de pages: 812
Coordonn�es du fabricant: ProductSafety@springernature.com
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Metasomatism and the Chemical Transformation of Rock: The Role of Fluids in Terrestrial and Extraterrestrial Processes (Lecture Notes in Earth System Sciences)

Harlov, Daniel; Austrheim, Hakon

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Metasomatism and the Chemical Transformation of Rock

Daniel Harlov|Hakon Austrheim

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ISBN 10 : 3662520648 ISBN 13 : 9783662520642

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Metasomatism and the Chemical Transformation of Rock

Hakon Austrheim

Edit� par Springer Berlin Heidelberg Aug 2016, 2016

ISBN 10 : 3662520648 ISBN 13 : 9783662520642

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Taschenbuch. Etat : Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -Fluid-aided mass transfer and subsequent mineral re-equilibration are the two defining features of metasomatism and must be present in order for metamorphism to occur. Coupled with igneous and tectonic processes, metasomatism has played a major role in the formation of the Earth's continental and oceanic crust and lithospheric mantle as well as in their evolution and subsequent stabilization. Metasomatic processes can include ore mineralization, metasomatically induced alteration of oceanic lithosphere, mass transport in and alteration of subducted oceanic crust and overlying mantle wedge, which has subsequent implications regarding mass transport, fluid flow, and volatile storage in the lithospheric mantle overall, as well as both regional and localized crustal metamorphism. Metasomatic alteration of accessory minerals such as zircon or monazite can allow for the dating of metasomatic events as well as give additional information regarding the chemistry of the fluids responsible. Lastly present day movement of fluids in both the lithospheric mantle and deep to mid crust can be observed utilizing geophysical resources such as electrical resistivity and seismic data. Such observations help to further clarify the picture of actual metasomatic processes as inferred from basic petrographic, mineralogical, and geochemical data. The goal of this volume is to bring together a diverse group of geologists, each of whose specialities and long range experience regarding one or more aspects of metasomatism during geologic processes, should allow them to contribute to a series of review chapters, which outline the basis of our current understanding of how metasomatism influences and helps to control both the evolution and stability of the crust and lithospheric mantle. 812 pp. Englisch. N� de r�f. du vendeur 9783662520642

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Metasomatism and the Chemical Transformation of Rock: The Role of Fluids in Terrestrial and Extraterrestrial Processes (eng)

Harlov, Daniel

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Metasomatism and the Chemical Transformation of Rock: The Role of Fluids in Terrestrial and Extraterrestrial Processes (Lecture Notes in Earth System Sciences)

Harlov, Daniel; Austrheim, Hakon

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Metasomatism and the Chemical Transformation of Rock | The Role of Fluids in Terrestrial and Extraterrestrial Processes

Daniel Harlov (u. a.)

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Metasomatism and the Chemical Transformation of Rock: The Role of Fluids in Terrestrial and Extraterrestrial Processes (Lecture Notes in Earth System Sciences)

Harlov, Daniel; Austrheim, Hakon

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Metasomatism and the Chemical Transformation of Rock: The Role of Fluids in Terrestrial and Extraterrestrial Processes (Lecture Notes in Earth System Sciences)

Harlov, Daniel; Austrheim, Hakon

Edit� par Springer, 2016

ISBN 10 : 3662520648 ISBN 13 : 9783662520642

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Metasomatism and the Chemical Transformation of Rock

Daniel Harlov

Edit� par Springer, Springer Aug 2016, 2016

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Taschenbuch. Etat : Neu. This item is printed on demand - Print on Demand Titel. Neuware -Fluid-aided mass transfer and subsequent mineral re-equilibration are the two defining features of metasomatism and must be present in order for metamorphism to occur. Coupled with igneous and tectonic processes, metasomatism has played a major role in the formation of the Earth�s continental and oceanic crust and lithospheric mantle as well as in their evolution and subsequent stabilization. Metasomatic processes can include ore mineralization, metasomatically induced alteration of oceanic lithosphere, mass transport in and alteration of subducted oceanic crust and overlying mantle wedge, which has subsequent implications regarding mass transport, fluid flow, and volatile storage in the lithospheric mantle overall, as well as both regional and localized crustal metamorphism. Metasomatic alteration of accessory minerals such as zircon or monazite can allow for the dating of metasomatic events as well as give additional information regarding the chemistry of the fluids responsible. Lastly present day movement of fluids in both the lithospheric mantle and deep to mid crust can be observed utilizing geophysical resources such as electrical resistivity and seismic data. Such observations help to further clarify the picture of actual metasomatic processes as inferred from basic petrographic, mineralogical, and geochemical data. The goal of this volume is to bring together a diverse group of geologists, each of whose specialities and long range experience regarding one or more aspects of metasomatism during geologic processes, should allow them to contribute to a series of review chapters, which outline the basis of our current understanding of how metasomatism influences and helps to control both the evolution and stability of the crust and lithospheric mantle.Springer-Verlag KG, Sachsenplatz 4-6, 1201 Wien 812 pp. Englisch. N� de r�f. du vendeur 9783662520642

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Metasomatism and the Chemical Transformation of Rock : The Role of Fluids in Terrestrial and Extraterrestrial Processes

Hakon Austrheim

Edit� par Springer Berlin Heidelberg, 2016

ISBN 10 : 3662520648 ISBN 13 : 9783662520642

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Taschenbuch. Etat : Neu. Druck auf Anfrage Neuware - Printed after ordering - Fluid-aided mass transfer and subsequent mineral re-equilibration are the two defining features of metasomatism and must be present in order for metamorphism to occur. Coupled with igneous and tectonic processes, metasomatism has played a major role in the formation of the Earth's continental and oceanic crust and lithospheric mantle as well as in their evolution and subsequent stabilization. Metasomatic processes can include ore mineralization, metasomatically induced alteration of oceanic lithosphere, mass transport in and alteration of subducted oceanic crust and overlying mantle wedge, which has subsequent implications regarding mass transport, fluid flow, and volatile storage in the lithospheric mantle overall, as well as both regional and localized crustal metamorphism. Metasomatic alteration of accessory minerals such as zircon or monazite can allow for the dating of metasomatic events as well as give additional information regarding the chemistry of the fluids responsible. Lastly present day movement of fluids in both the lithospheric mantle and deep to mid crust can be observed utilizing geophysical resources such as electrical resistivity and seismic data. Such observations help to further clarify the picture of actual metasomatic processes as inferred from basic petrographic, mineralogical, and geochemical data. The goal of this volume is to bring together a diverse group of geologists, each of whose specialities and long range experience regarding one or more aspects of metasomatism during geologic processes, should allow them to contribute to a series of review chapters, which outline the basis of our current understanding of how metasomatism influences and helps to control both the evolution and stability of the crust and lithospheric mantle. N� de r�f. du vendeur 9783662520642

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