Metasomatism In Oceanic And Continental Lithospheric Mantle
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Metasomatism in Oceanic and Continental Lithospheric Mantle
Author | : Massimo Coltorti,Michel Grégoire |
Publsiher | : Geological Society of London |
Total Pages | : 376 |
Release | : 2008 |
Genre | : Nature |
ISBN | : 1862392420 |
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Metasomatism and the Chemical Transformation of Rock
Author | : Daniel Harlov,Hakon Austrheim |
Publsiher | : Springer Science & Business Media |
Total Pages | : 804 |
Release | : 2012-08-14 |
Genre | : Science |
ISBN | : 9783642283932 |
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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.
Metasomatism and the Chemical Transformation of Rock
Author | : Daniel Harlov,Hakon Austrheim |
Publsiher | : Springer |
Total Pages | : 806 |
Release | : 2012-08-15 |
Genre | : Science |
ISBN | : 3642283950 |
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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.
Petrological Evolution of the European Lithospheric Mantle
Author | : Massimo Coltorti |
Publsiher | : Geological Society of London |
Total Pages | : 260 |
Release | : 2010 |
Genre | : Basalt |
ISBN | : 1862393044 |
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Selected conference papers from the European Mantle Workshop, EMAW, held Ferrara, 2007.
Mantle Metasomatism
Author | : Martin A. Menzies,C. J. Hawkesworth |
Publsiher | : Unknown |
Total Pages | : 508 |
Release | : 1987 |
Genre | : Earth |
ISBN | : UCSD:31822002389153 |
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Continental Mantle
Author | : Martin A. Menzies |
Publsiher | : Oxford University Press, USA |
Total Pages | : 214 |
Release | : 1990 |
Genre | : Continents |
ISBN | : UCSD:31822005134515 |
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Very Good,No Highlights or Markup,all pages are intact.
Volcanism and Evolution of the African Lithosphere
Author | : Luigi Beccaluva,Gianluca Bianchini,B. Marjorie Wilson |
Publsiher | : Geological Society of America |
Total Pages | : 342 |
Release | : 2011-01-01 |
Genre | : Science |
ISBN | : 9780813724782 |
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The Earth s Heterogeneous Mantle
Author | : Amir Khan,Frédéric Deschamps |
Publsiher | : Springer |
Total Pages | : 530 |
Release | : 2015-04-28 |
Genre | : Science |
ISBN | : 9783319156279 |
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This book highlights and discusses recent developments that have contributed to an improved understanding of observed mantle heterogeneities and their relation to the thermo-chemical state of Earth's mantle, which ultimately holds the key to unlocking the secrets of the evolution of our planet. This series of topical reviews and original contributions address 4 themes. Theme 1 covers topics in geophysics, including global and regional seismic tomography, electrical conductivity and seismic imaging of mantle discontinuities and heterogeneities in the upper mantle, transition zone and lower mantle. Theme 2 addresses geochemical views of the mantle including lithospheric evolution from analysis of mantle xenoliths, composition of the deep Earth and the effect of water on subduction-zone processes. Theme 3 discusses geodynamical perspectives on the global thermo-chemical structure of the deep mantle. Theme 4 covers application of mineral physics data and phase equilibrium computations to infer the regional-scale thermo-chemical structure of the mantle.