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A New Model for Estimating Deep-Level Magma Ascent Rates from Thermobarometry : An Example form Mt. Etna and Implications for Deep-Seated Magma Dehydratation
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Is part of
Acta vulcanologica : Journal of the National Volcanic Group of Italy : 20/21, 1/2, 2008/2009-
Information
DOI: 10.1400/146024
ISSN: 1724-0425
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In this issue
- Fabrizio Innocenti (1939-2009)
- The Late Miocene Intrusive Complex of Elba Island
- The 40-Year Contribution of Fabrizio Innocenti to Understanding the Geodynamic Evolution of the Eastern Mediterranean
- 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
- Cenozoic Volcanic Activity in Greece
- Geological Map (Scale 1:50,000) if Limnos Island (Greece)
- Paleogene Ultrapotassic Volcanic Rocks of the Eastern Rhodopes (Southern Bulgaria)
- Genesis of Analcime and Nepheline-Potassium Feldspar-Kalsilite Intergrowths
- The Volcano-tectonic Activity of the Main Ethiopian Rift (East Africa)
- 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
- The Radicofani Volcano
- The Subduction Factory of the Aeolian Volcanic Arc.
- The Early Paleozoic Antarctic Margin of Gondwana
- The Cenozoic Basalts form Central-Southern Patagonia
- Charles Darwin Geologist at Santiago (Cape Verde Islands)
