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Autor(en): 
  • Anthony Dosseto
  • Simon P. Turner
  • James A. Van-Orman
  • Timescales of Magmatic Processes: From Core to Atmosphere 
     

    (Buch)
    Dieser Artikel gilt, aufgrund seiner Grösse, beim Versand als 2 Artikel!


    Übersicht

    Auf mobile öffnen
     
    Lieferstatus:   Auf Bestellung (Lieferzeit unbekannt)
    Veröffentlichung:  November 2010  
    Genre:  Naturwissensch., Medizin, Technik 
     
    Earth Sciences / Geomorphologie / Geowissenschaften / Igneous & Metamorphic Petrology and Volcanology / Petrologie u. Vulkanologie eruptiver u. metamorpher Systeme
    ISBN:  9781444332612 
    EAN-Code: 
    9781444332612 
    Verlag:  Wiley 
    Einband:  Kartoniert  
    Sprache:  English  
    Dimensionen:  H 248 mm / B 189 mm / D 17 mm 
    Gewicht:  702 gr 
    Seiten:  272 
    Bewertung: Titel bewerten / Meinung schreiben
    Inhalt:
    Quantifying the timescales of current geological processes is critical for constraining the physical mechanisms operating on the Earth today. Since the Earth's origin 4.55 billion years ago magmatic processes have continued to shape the Earth, producing the major reservoirs that exist today (core, mantle, crust, oceans and atmosphere) and promoting their continued evolution. But key questions remain. When did the core form and how quickly? How are magmas produced in the mantle, and how rapidly do they travel towards the surface? How long do magmas reside in the crust, differentiating and interacting with the host rocks to yield the diverse set of igneous rocks we see today? How fast are volcanic gases such as carbon dioxide released into the atmosphere? This book addresses these and other questions by reviewing the latest advances in a wide range of Earth Science disciplines: from the measurement of short-lived radionuclides to the study of element diffusion in crystals and numerical modelling of magma behaviour. It will be invaluable reading for advanced undergraduate and graduate students, as well as igneous petrologists, mineralogists and geochemists involved in the study of igneous rocks and processes.

      



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