Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8911516 | Lithos | 2018 | 13 Pages |
Abstract
Sr-O mixing models indicate that such magmas were derived from a mantle source that was contaminated by up to 10% of a 1:1 mixture of pelagic and carbonate sediments. These findings together demonstrate the highly complex and varied magma sources in the Campania volcanic district. Triple oxygen isotope variations (Î17O), based on measurements of both 18O/16O and 17O/16O ratios in potential assimilants are in agreement with these conclusions.
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Earth and Planetary Sciences
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Authors
Raffaella Silvia Iovine, Fabio Carmine Mazzeo, Gerhard Wörner, Carlo Pelullo, Gianluca Cirillo, Ilenia Arienzo, Andreas Pack, Massimo D'Antonio,