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Vittorio Zanon and Maria Luce Frezzotti Magma storage and ascent conditions beneath Pico and Faial islands (Azores archipelago): A study on fluid inclusions Geochemistry, Geophysics, Geosystems 14

Version of Record online: 3 SEP 2013 | DOI: 10.1002/ggge.20221

Key Points

  • Magma ponding and crystallization areas are at the crust-mantle boundary
  • Shallow-level magma reservoirs can form in response to tectonic stress
  • Tectonic stress determines either rapid magma extraction or its underplating

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