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Taschenbuch. Condizione: 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. …

Buch. Condizione: 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. …

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Buch. Condizione: Neu. Druck auf Anfrage Neuware - Printed after ordering - This book compiles a compendium of the current knowledge on the distribution, speciation and behavior of sulfur in the atmosphere, surface, crust, mantle, and core of the Earth as well as the other bodies of the solar system, including the terrestrial planets, dwarf planets, asteroids, moons, and the gas giants. It brings together a diverse group of geoscientists with broad interests, knowledge, and expertise regarding the behavior of sulfur in a variety of natural processes. This diversity of knowledge and experience allowed them to contribute to a comprehensive and coherent series of review chapters, which outline and expand upon the basis of our current understanding regarding how sulfur contributes to the origin, evolution, and functioning of the Earth as well as the other bodies of the solar system.With a plethora of oxidation states (from -2 to +6), a cosmic element abundance rank of ten, a fascinating redox-, pH-, and radical-dependent chemistry, a strong chemical affinity for many metals, and a large fractionation among its four stable isotopes, sulfur is a key player and a powerful tracer element in the various physical and chemical processes occurring in the atmosphere, surface, crust, mantle, and core of the Earth as well as in the other bodies of the solar system. On Earth, as a key component of aqueous fluids, sulfur is a powerful complexing agent for a series of metals, which allows for their transfer across the lithosphere and subsequent concentration as ore deposits. As sulfur dioxide and sulfate, sulfur can act as an oxidizing agent, whereas as hydrogen sulfide and polysulfides, it can act as a reducing agent and a strong binder for metals, over a wide range of pressures and temperatures in the crust, upper mantle, and during subduction processes. Sulfur controls the partitioning of a many metals between silicate melts, gaseous and aqueous fluids, and mineral phases, thereby playing a major role in the formation of magmatic-hydrothermal and metamorphic ore deposits that supply strategic metal resources to our society. In the atmospheres of both the terrestrial worlds and the gas giants, sulfur plays a diverse and important role shaping their physical, chemical and biological evolution.…

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Taschenbuch. Condizione: Neu. Druck auf Anfrage Neuware - Printed after ordering - The book summarizes the knowledge and experiences concerning the role of halogens during various geochemical processes, such as diagenesis, ore-formation, magma evolution, metasomatism, mineralization, and metamorphism in the crust and mantle of the Earth. It comprises the role of halogens in other terrestrial worlds like volatile-rich asteroids, Mars, and the ice moons of Jupiter and Saturn. Review chapters outline and expand upon the basis of our current understanding regarding how halogens contribute to the geochemical/geophysical evolution and stability of terrestrial worlds overall.…

Buch. Condizione: Neu. Druck auf Anfrage Neuware - Printed after ordering - The book summarizes the knowledge and experiences concerning the role of halogens during various geochemical processes, such as diagenesis, ore-formation, magma evolution, metasomatism, mineralization, and metamorphism in the crust and mantle of the Earth. It comprises the role of halogens in other terrestrial worlds like volatile-rich asteroids, Mars, and the ice moons of Jupiter and Saturn. Review chapters outline and expand upon the basis of our current understanding regarding how halogens contribute to the geochemical/geophysical evolution and stability of terrestrial worlds overall.…

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Buch. Condizione: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -This book compiles a compendium of the current knowledge on the distribution, speciation and behavior of sulfur in the atmosphere, surface, crust, mantle, and core of the Earth as well as the other bodies of the solar system, including the terrestrial planets, dwarf planets, asteroids, moons, and the gas giants. It brings together a diverse group of geoscientists with broad interests, knowledge, and expertise regarding the behavior of sulfur in a variety of natural processes. This diversity of knowledge and experience allowed them to contribute to a comprehensive and coherent series of review chapters, which outline and expand upon the basis of our current understanding regarding how sulfur contributes to the origin, evolution, and functioning of the Earth as well as the other bodies of the solar system.With a plethora of oxidation states (from -2 to +6), a cosmic element abundance rank of ten, a fascinating redox-, pH-, and radical-dependent chemistry, a strong chemical affinity for many metals, and a large fractionation among its four stable isotopes, sulfur is a key player and a powerful tracer element in the various physical and chemical processes occurring in the atmosphere, surface, crust, mantle, and core of the Earth as well as in the other bodies of the solar system. On Earth, as a key component of aqueous fluids, sulfur is a powerful complexing agent for a series of metals, which allows for their transfer across the lithosphere and subsequent concentration as ore deposits. As sulfur dioxide and sulfate, sulfur can act as an oxidizing agent, whereas as hydrogen sulfide and polysulfides, it can act as a reducing agent and a strong binder for metals, over a wide range of pressures and temperatures in the crust, upper mantle, and during subduction processes. Sulfur controls the partitioning of a many metals between silicate melts, gaseous and aqueous fluids, and mineral phases, thereby playing a major role in the formation of magmatic-hydrothermal and metamorphic ore deposits that supply strategic metal resources to our society. In the atmospheres of both the terrestrial worlds and the gas giants, sulfur plays a diverse and important role shaping their physical, chemical and biological evolution. 1536 pp. Englisch.…

Taschenbuch. Condizione: 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.…

Buch. Condizione: 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. …

Buch. Condizione: Neu. This item is printed on demand - Print on Demand Titel. Neuware -This book compiles a compendium of the current knowledge on the distribution, speciation and behavior of sulfur in the atmosphere, surface, crust, mantle, and core of the Earth as well as the other bodies of the solar system, including the terrestrial planets, dwarf planets, asteroids, moons, and the gas giants. It brings together a diverse group of geoscientists with broad interests, knowledge, and expertise regarding the behavior of sulfur in a variety of natural processes. This diversity of knowledge and experience allowed them to contribute to a comprehensive and coherent series of review chapters, which outline and expand upon the basis of our current understanding regarding how sulfur contributes to the origin, evolution, and functioning of the Earth as well as the other bodies of the solar system.With a plethora of oxidation states (from ¿2 to +6), a cosmic element abundance rank of ten, a fascinating redox¿, pH¿, and radical¿dependent chemistry, a strong chemical affinity for many metals, and a large fractionation among its four stable isotopes, sulfur is a key player and a powerful tracer element in the various physical and chemical processes occurring in the atmosphere, surface, crust, mantle, and core of the Earth as well as in the other bodies of the solar system. On Earth, as a key component of aqueous fluids, sulfur is a powerful complexing agent for a series of metals, which allows for their transfer across the lithosphere and subsequent concentration as ore deposits. As sulfur dioxide and sulfate, sulfur can act as an oxidizing agent, whereas as hydrogen sulfide and polysulfides, it can act as a reducing agent and a strong binder for metals, over a wide range of pressures and temperatures in the crust, upper mantle, and during subduction processes. Sulfur controls the partitioning of a many metals between silicate melts, gaseous and aqueous fluids, and mineral phases, thereby playing a major role in the formation of magmatic¿hydrothermal and metamorphic ore deposits that supply strategic metal resources to our society. In the atmospheres of both the terrestrial worlds and the gas giants, sulfur plays a diverse and important role shaping their physical, chemical and biological evolution.Springer Nature Customer Service Center GmbH, Europaplatz 3,69115 Heidelberg, Germany, Heidelberg 1540 pp. Englisch.…