Author: Frank Wigglesworth ClarkePublisher:
ISBN:
Category : Earth
Languages : en
Pages : 132
Book Description
The Composition of the Earth's Crust
Author: Frank Wigglesworth ClarkePublisher:
ISBN:
Category : Earth
Languages : en
Pages : 132
Book Description
The Earth's Crust and Upper Mantle
Author: Pembroke J. HartPublisher: American Geophysical Union
ISBN: 0875900135
Category : Science
Languages : en
Pages : 801
Book Description
Chemistry of the Earth's Crust
Author: Aleksandr Pavlovič VinogradovPublisher:
ISBN:
Category : Earth
Languages : en
Pages : 474
Book Description
The Chemistry of the Earth's Crust
Author: Henry Stephens WashingtonPublisher:
ISBN:
Category : Geochemistry
Languages : en
Pages : 64
Book Description
From Crust to Core
Author: Simon MittonPublisher: Cambridge University Press
ISBN: 1108426697
Category : Nature
Languages : en
Pages : 383
Book Description
A fascinating historical account of the emergence and development of the new interdisciplinary field of deep carbon science.
The Earth's Sedimentary Shell
Author: Aleksandr Borisovich RonovPublisher: Amer Geological Institute
ISBN:
Category : Science
Languages : en
Pages : 96
Book Description
Chemistry of the Earth's Crust
Author: Institut geokhimii i analiticheskoĭ khimii im. V.I. VernadskogoPublisher:
ISBN:
Category : Earth
Languages : en
Pages : 726
Book Description
Metasomatism and the Chemical Transformation of Rock
Author: Daniel HarlovPublisher: Springer Science & Business Media
ISBN: 3642283934
Category : Science
Languages : en
Pages : 804
Book Description
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.
The Chemistry of the Earth's Crust
Author: Henry Stephens WashingtonPublisher:
ISBN:
Category :
Languages : en
Pages :
Book Description
Hydrocarbon Habitat in Rift Basins
Author: J. J. LambiasePublisher: Geological Society of America
ISBN:
Category : Nature
Languages : en
Pages : 404
Book Description