Mantle Plumes A Multidisciplinary Approach /

The concept of mantle plumes, originally suggested by Morgan (1971), is widely but not unequivocally accepted as the cause for hotspot volcanism. Plumes are thought of as deep-rooted, approximately cylindrical regions of hot rising mantle rock with a typical diameter of 100-200 km. Pressure-release...

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Detalles Bibliográficos
Clasificación:Libro Electrónico
Autor Corporativo: SpringerLink (Online service)
Otros Autores: Ritter, Joachim R. R. (Editor ), Christensen, U.R (Editor )
Formato: Electrónico eBook
Idioma:Inglés
Publicado: Berlin, Heidelberg : Springer Berlin Heidelberg : Imprint: Springer, 2007.
Edición:1st ed. 2007.
Temas:
Geophysics.
Inorganic chemistry.
Geology.
Mathematical physics.
Inorganic Chemistry.
Theoretical, Mathematical and Computational Physics.
Acceso en línea:Texto Completo
Tabla de Contenidos:
  • Basic Properties of Mantle Plumes
  • Fluid Dynamics of Mantle Plumes
  • Case studies
  • Tracing the Hawaiian Mantle Plume by Converted Seismic Waves
  • Iceland: The current picture of a ridge-centred mantle plume
  • Combined Gas-geochemical and Receiver Function Studies of the Vogtland/NW Bohemia Intraplate Mantle Degassing Field, Central Europe
  • Crustal and Upper Mantle Structure of the French Massif Central Plume
  • Eifel Region
  • Geodynamic Setting of the Tertiary Hocheifel Volcanism (Germany), Part I: 40Ar/39Ar geochronology
  • Geodynamic Setting of the Tertiary Hocheifel Volcanism (Germany), Part II: Geochemistry and Sr, Nd and Pb Isotopic Compositions
  • The Quaternary Volcanic Fields of the East and West Eifel (Germany)
  • Thermal and Geochemical Evolution of the Shallow Subcontinental Lithospheric Mantle Beneath the Eifel: Constraints from Mantle Xenoliths, a Review
  • He-Ne-Ar Isotope Systematics of Eifel and Pannonian Basin Mantle Xenoliths Trace Deep Mantle Plume-Lithosphere Interaction Beneath the European Continent
  • Quaternary Uplift in the Eifel Area
  • The Seismic Signature of the Eifel Plume
  • Upper Mantle Structure Beneath the Eifel from Receiver Functions
  • Rayleigh Wave Dispersion in the Eifel Region
  • Seismic Anisotropy in the Asthenosphere Beneath the Eifel Region, Western Germany
  • Gravity Observations in the Western Rhenish Massif and Forward Modelling of the Eifel Plume Bouguer Anomaly.

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