Dear Colleagues,
Arc evolution: space, time, morphology, and longevity of volcanic arcs
Arc settings are foundries in which heat, mass, and fluid transfer processes contribute to constructing the continental crust, feeding volcanic eruptions, and maintaining a hydrosphere and atmosphere on Earth. Volcanic edifices in arcs span a wide range in morphology, volume, and eruptive longevity, reflecting temporal and spatial variations in melt extraction processes within the Earth’s lithosphere. To date, constraints on the production and eruption of magmas, the modulation of volcanism by tectonic and landscape evolutionary processes, and the links amongst the dynamics of the mantle, crust and surface do not fully explain the factors controlling the eruptive volume, spatial, temporal and compositional variability of eruptions at a given volcano or at an arc scale.
Severine Moune, Laboratoire Magmas et Volcans, OPGC-UCA, France; S.Moune@xxxxxxxxx-bpcl
Mattia Pistone, Smithsonian Institution National Museum of Natural History; PistoneM@xxxxxx
Mark Jellinek, EOAS, University of British Columbia; mjellinek@xxxxxxxxxx
Leif Karlstrom, University of Oregon, leif@xxxxxxxxxxx
Diana C. Roman, Department of Terrestrial Magnetism Carnegie Institution for Science; droman@xxxxxxxxxxx
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