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

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書目名稱Metasomatism and the Chemical Transformation of Rock
副標題The Role of Fluids i
編輯Daniel E. Harlov,H?kon Austrheim
視頻videohttp://file.papertrans.cn/632/631738/631738.mp4
概述A 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
叢書名稱Lecture Notes in Earth System Sciences
圖書封面Titlebook: Metasomatism and the Chemical Transformation of Rock; The Role of Fluids i Daniel E. Harlov,H?kon Austrheim Book 2013 Springer-Verlag Berli
描述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 observatio
出版日期Book 2013
關鍵詞Fluid; Geochemistry; Mass-transfer; Metamorphism; Metasomatism
版次1
doihttps://doi.org/10.1007/978-3-642-28394-9
isbn_softcover978-3-662-52064-2
isbn_ebook978-3-642-28394-9Series ISSN 2193-8571 Series E-ISSN 2193-858X
issn_series 2193-8571
copyrightSpringer-Verlag Berlin Heidelberg 2013
The information of publication is updating

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Thermodynamic Modeling and Thermobarometry of Metasomatized Rocks,e crust. However, application of thermodynamic modeling to metasomatized rocks is not without pitfalls. As with “normal” metamorphic rocks, the main difficulty is to select mineral compositions that were in equilibrium during their crystallization. This essential task is particularly difficult in me
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Structural Controls of Metasomatism on a Regional Scale,l, and may be intrinsic or the result of deformation processes such as micro-fracturing (e.g. grain boundary sliding), fracturing, faulting, foliation and shear zone development, and hydro-fracturing. Chromatographic theory has been developed to explain metasomatic zonation, and applies not only whe
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Metasomatism Within the Ocean Crust,osition of the oceans and their rocky foundation. Although the overall exchange fluxes are great, the first-order metasomatic changes of crustal rocks are generally minor (usually <10% relative change in major element concentrations). Drastic fluid-induced metasomatic mass transfers are limited to a
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Metasomatism in Subduction Zones of Subducted Oceanic Slabs, Mantle Wedges, and the Slab-Mantle Intts in subduction zones, with larger scale manifestations including the metasomatism related to mass flux leading to arc magmatism and convergent margin volatiles cycling. Subduction-zone metasomatism is initiated at very shallow levels, as oceanic slabs entering trenches bend and are potentially inf
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Metasomatism During High-Pressure Metamorphism: Eclogites and Blueschist-Facies Rocks,ing constraints on the P-T conditions, composition, and type of slab-derived fluids responsible for metasomatism in subduction zone environments since they are the only direct witnesses of such processes. Usually, solute-poor, aqueous fluids, derived by prograde HP metamorphic devolatilisation react
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