Titlebook: Metasomatism and the Chemical Transformation of Rock; The Role of Fluids i Daniel E. Harlov,Håkon Austrheim Book 2013 Springer-Verlag Berli

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Mantle Metasomatism,s), brought to the surface of in basaltic to kimberlitic magmas, became widespread. Two main types of metasomatism were defined: modal (or patent) metasomatism describes the introduction of new minerals; cryptic metasomatism describes changes in composition of pre-existing minerals without formation

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Mapping the Distribution of Fluids in the Crust and Lithospheric Mantle Utilizing Geophysical Metho mantle to be mapped. This is in contrast to geological studies that investigate mid-crustal rocks have been exhumed and fluids associated with metasomatism are absent. The primary geophysical methods that can be used are (a) electromagnetic methods that image electrical resistivity and (b) seismic

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A Hydromechanical Model for Lower Crustal Fluid Flow,at fluid generation and compaction operate on the same time scale at low metamorphic grade, even in rocks that are deforming by ductile mechanisms in response to tectonic stress. However, thermally-activated viscous compaction may dominate fluid flow patterns at moderate to high metamorphic grades.

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Metasomatism in the Early Solar System: The Record from Chondritic Meteorites,e earliest stages of Solar System evolution. The exact nature of these processes, as well as the conditions and environments where metasomatism occurred, are still the subject of vigorous debate. The interaction of aqueous fluids with early Solar System solids affected different chondrite groups to

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https://doi.org/10.1007/978-3-642-28394-9Fluid; Geochemistry; Mass-transfer; Metamorphism; Metasomatism

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Daniel E. Harlov,Håkon AustrheimA complete state-of-the-art review of metasomatism.Written by leading experts in the field.Reviews metasomatic processes in the Earth‘s Crust and Mantle as well as chondritic meteorites

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Effects of Metasomatism on Mineral Systems and Their Host Rocks: Alkali Metasomatism, Skarns, Greisnt, but also in the transport of volatile components, which are responsible for metasomatic processes. Some of the most impressive results of these processes are, for example, fenites (K- and Na-metasomatism), skarns (Ca-metasomatism) and tourmalinisation (B-metasomatism).

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