Fluid Movements — Element Transport and the Composition of the Deep Crust: Nato Science Series C:, cartea 281
Autor David Bridgwateren Limba Engleză Paperback – 26 sep 2011
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Specificații
ISBN-13: 9789401069359
ISBN-10: 9401069352
Pagini: 440
Ilustrații: 436 p.
Dimensiuni: 155 x 235 x 23 mm
Greutate: 0.61 kg
Ediția:Softcover reprint of the original 1st ed. 1989
Editura: SPRINGER NETHERLANDS
Colecția Springer
Seria Nato Science Series C:
Locul publicării:Dordrecht, Netherlands
ISBN-10: 9401069352
Pagini: 440
Ilustrații: 436 p.
Dimensiuni: 155 x 235 x 23 mm
Greutate: 0.61 kg
Ediția:Softcover reprint of the original 1st ed. 1989
Editura: SPRINGER NETHERLANDS
Colecția Springer
Seria Nato Science Series C:
Locul publicării:Dordrecht, Netherlands
Public țintă
ResearchCuprins
Magmas as a source of heat and fluids in granulite facies metamorphism..- Morphology of granulite — amphibolite facies transitions: The importance of fluid movements..- Contrasting mechanisms of charnockite formation in the amphibolite to granulite grade transition zones of southern India..- Chemical changes associated with formation of granulite and migration of complex C-O-H-S fluids, Sri Lanka..- Metamorphism and melting at an exposed example of the Conrad discontinuity, Kapuskasing uplift, Canada..- Melt-induced fluid pumping and the source of CO2 in granulites..- P-T and fluid evolution of the Angmagssalik “charnockite” complex, SE Greenland..- Processes of formation and retrogression of Scourian granulites..- Proterozoic metasediments from the deep crust of Rogaland, SW Norway: Chemistry of metabasites and granofelses..- Limited fluid transport from the gneiss core toward the schist envelope of the dome de L’Agout, France..- Hydrothermal graphite veins and Acadian granulite facies metamorphism New Hampshire, USA..- The crustal origin of eclogite - static or dynamic..- Retrogression and fluid movement across a granulite-amphibolite facies boundary in middle Archaean Nuk gneisses, Fiskefjord, southern West Greenland..- Mineral changes, element mobility, and fluids associated with deep shearing in the Mount Helen structural belt, Wyoming, U.S.A..- The Ataneq fault and mid-Proterozoic retrograde metamorphism of early Archaean tonalites of the Isukasia area, southern West Greenland: Reactions, fluid compositions and implications for regional studies..- Deformation and mass transport in the Nordre Strømfjord shear zone, Central West Greenland..- Metasomatic alteration of ultramafic rocks..- Mass balance of a gabbroic rock-amphibolite transition..- Mass transferrelated to ductile shear zone development in a metagabbro..- Incorporation of Rb in muscovite during progressive medium grade metamorphism. An interpretation of experimental results..- Fluid control on emplacement of sialic magmas during Archaean crustal accretion..- The isotopic characterisation of aqueous and leucogranitic crustal fluids..- Stable isotope fronts and crustal buffering - 1 dimensional mass balance and kinetics..- The effect of fluid-controlled element mobility during metamorphism on whole rock isotope systems, some theoretical aspects and possible examples..- On the possible role of fluid transport in the distribution of U and Pb in an Archaean gneiss complex..- Reappraisal of crustal evolution at Kangimut sammisoq, Ameralik fjord, southern West Greenland: Fluid movement and interpretation of Pb/Pb isotopic data..- Changes in the isotopic composition of whole-rock Pb during different stages of retrogression of late Archaean granulite facies gneisses from Kangimut sammisoq, southern West Greenland..- Diffusion and/or plastic deformation around fluid inclusions in synthetic quartz: New investigations..- Permeability, bulk modulus and complex resistivity in crystalline rocks..- Rock-fluid interaction: interpetation by zeta potential and complex resistivity measurements..