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Metasomatism and the Chemical Transformation of Rock - The Role of Fluids in Terrestrial and Extraterrestrial Processes (Paperback, Softcover reprint of the original 1st ed. 2013)
Loot Price: R5,901
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Metasomatism and the Chemical Transformation of Rock - The Role of Fluids in Terrestrial and Extraterrestrial Processes (Paperback, Softcover reprint of the original 1st ed. 2013)
Series: Lecture Notes in Earth System Sciences
Expected to ship within 10 - 15 working days
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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.
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