Metasomatism In Oceanic And Continental Lithospheric Mantle
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Author |
: Massimo Coltorti |
Publisher |
: Geological Society of London |
Total Pages |
: 376 |
Release |
: 2008 |
ISBN-10 |
: 1862392420 |
ISBN-13 |
: 9781862392427 |
Rating |
: 4/5 (20 Downloads) |
Synopsis Metasomatism in Oceanic and Continental Lithospheric Mantle by : Massimo Coltorti
Author |
: Daniel Harlov |
Publisher |
: Springer Science & Business Media |
Total Pages |
: 804 |
Release |
: 2012-08-14 |
ISBN-10 |
: 9783642283932 |
ISBN-13 |
: 3642283934 |
Rating |
: 4/5 (32 Downloads) |
Synopsis Metasomatism and the Chemical Transformation of Rock by : Daniel Harlov
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.
Author |
: Daniel Harlov |
Publisher |
: Springer |
Total Pages |
: 806 |
Release |
: 2012-08-15 |
ISBN-10 |
: 3642283950 |
ISBN-13 |
: 9783642283956 |
Rating |
: 4/5 (50 Downloads) |
Synopsis Metasomatism and the Chemical Transformation of Rock by : Daniel Harlov
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.
Author |
: Martin A. Menzies |
Publisher |
: |
Total Pages |
: 508 |
Release |
: 1987 |
ISBN-10 |
: UCSD:31822002389153 |
ISBN-13 |
: |
Rating |
: 4/5 (53 Downloads) |
Synopsis Mantle Metasomatism by : Martin A. Menzies
Author |
: Martin A. Menzies |
Publisher |
: |
Total Pages |
: 468 |
Release |
: 1988 |
ISBN-10 |
: UCSD:31822007465388 |
ISBN-13 |
: |
Rating |
: 4/5 (88 Downloads) |
Synopsis Oceanic and Continental Lithosphere by : Martin A. Menzies
Author |
: Jian Wang |
Publisher |
: |
Total Pages |
: 320 |
Release |
: 2007 |
ISBN-10 |
: OCLC:658152793 |
ISBN-13 |
: |
Rating |
: 4/5 (93 Downloads) |
Synopsis Oxidation and Metasomatism of Lithospheric Mantle Beneath the Southern South America by : Jian Wang
Author |
: Martin A. Menzies |
Publisher |
: Oxford University Press, USA |
Total Pages |
: 214 |
Release |
: 1990 |
ISBN-10 |
: UCSD:31822005134515 |
ISBN-13 |
: |
Rating |
: 4/5 (15 Downloads) |
Synopsis Continental Mantle by : Martin A. Menzies
Very Good,No Highlights or Markup,all pages are intact.
Author |
: Huaiyu Yuan |
Publisher |
: John Wiley & Sons |
Total Pages |
: 240 |
Release |
: 2018-11-20 |
ISBN-10 |
: 9781119249719 |
ISBN-13 |
: 1119249716 |
Rating |
: 4/5 (19 Downloads) |
Synopsis Lithospheric Discontinuities by : Huaiyu Yuan
A multidisciplinary update on continental plate tectonics and plate boundary discontinuities Understanding the origin and evolution of the continental crust continues to challenge Earth scientists. Lithospheric Discontinuities offers a multidisciplinary review of fine scale layering within the continental lithosphere to aid the interpretation of geologic layers. Once Earth scientists can accurately decipher the history, internal dynamics, and evolution of the continental lithosphere, we will have a clearer understanding of how the crust formed, how plate tectonics began, and how our continents became habitable. Volume highlights: Theories and observations of the current state of tectonic boundaries and discontinuities Contributions on field observations, laboratory experiments, and geodynamic predictions from leading experts in the field Mantle fabrics in response to various mantle deformation processes Insights on fluid distribution using geophysical observations, and thermal and viscosity constraints from dynamic modeling Discontinuities associated with lithosphere and lithosphere-asthenosphere boundary An integrated study of the evolving physical and chemical processes associated with lithosphere asthenosphere interaction Written for academic and researchgeoscientists, particularly in the field of tectonophysics, geophysicists, geodynamics, seismology, structural geology, environmental geology, and geoengineering, Lithospheric Discontinuities is a valuable resource that sheds light on the origin and evolution of plate interaction processes.
Author |
: Peter H. Nixon |
Publisher |
: John Wiley & Sons |
Total Pages |
: 892 |
Release |
: 1987 |
ISBN-10 |
: MINN:31951000749448N |
ISBN-13 |
: |
Rating |
: 4/5 (8N Downloads) |
Synopsis Mantle Xenoliths by : Peter H. Nixon
The eruption of deep-seated xenoliths in basaltic, alnoitic, kimberlitic, etc volcanoes provides the geologist with an important direct means of examining the fragments of the earth's mantle and lower crust.
Author |
: Beth N. Orcutt |
Publisher |
: Cambridge University Press |
Total Pages |
: 687 |
Release |
: 2019-10-17 |
ISBN-10 |
: 9781108477499 |
ISBN-13 |
: 1108477496 |
Rating |
: 4/5 (99 Downloads) |
Synopsis Deep Carbon by : Beth N. Orcutt
A comprehensive guide to carbon inside Earth - its quantities, movements, forms, origins, changes over time and impact on planetary processes. This title is also available as Open Access on Cambridge Core.