A New Model for Estimating Deep-Level Magma Ascent Rates from Thermobarometry : An Example form Mt. Etna and Implications for Deep-Seated Magma Dehydratation

P. [1-13] [13]

• Artikel aus derselben Ausgabe (einzeln erhältlich)

  • Fabrizio Innocenti (1939-2009)
    Artikel abrufen
  • The Late Miocene Intrusive Complex of Elba Island
    Artikel abrufen
  • The 40-Year Contribution of Fabrizio Innocenti to Understanding the Geodynamic Evolution of the Eastern Mediterranean
    Artikel abrufen
  • Early Triassic Granitic Magmatism (Arnea and Kerkini Granitic Complezes) in the Vertiskos Unit (Serbo-Macedoniam Massif, North-Eastern Greece) and Its Significance in the Geodynamic Evolution of the Area
    Artikel abrufen
  • Cenozoic Volcanic Activity in Greece
    Artikel abrufen
  • Geological Map (Scale 1:50,000) if Limnos Island (Greece)
    Artikel abrufen
  • Paleogene Ultrapotassic Volcanic Rocks of the Eastern Rhodopes (Southern Bulgaria)
    Artikel abrufen
  • Genesis of Analcime and Nepheline-Potassium Feldspar-Kalsilite Intergrowths
    Artikel abrufen
  • The Volcano-tectonic Activity of the Main Ethiopian Rift (East Africa)
    Artikel abrufen
  • A New Model for Estimating Deep-Level Magma Ascent Rates from Thermobarometry
  • The Distribution of Paramagnetic Centers in Glass and Lavas from Eruptive Activity at Mt. Etna
    Artikel abrufen
  • The Radicofani Volcano
    Artikel abrufen
  • The Subduction Factory of the Aeolian Volcanic Arc.
    Artikel abrufen
  • The Early Paleozoic Antarctic Margin of Gondwana
    Artikel abrufen
  • The Cenozoic Basalts form Central-Southern Patagonia
    Artikel abrufen
  • Charles Darwin Geologist at Santiago (Cape Verde Islands)
    Artikel abrufen

  Mehr anzeigen
• Informationen

  DOI: 10.1400/146024

  ISSN: 1724-0425

  Permalink: http://digital.casalini.it/10.1400/146024