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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• Informationen

  DOI: 10.1400/146024

  ISSN: 1724-0425

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