Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8911523 | Lithos | 2018 | 54 Pages |
Abstract
In this scenario, the calc-alkaline magmas derived from partial melting of a mantle wedge modified by a subduction component, whereas the within-plate (OIB) magmas derived from a deeper, unmodified sub-slab mantle source. Mixing between calc-alkaline and within-plate magmas during their rise to the surface produced the Na-alkaline Cappadocia basalts. The very low rate of extension allowed within-plate magmas (OIB) to reach the surface after having interacted with the overlying calc-alkaline magmas in the late stages of Cappadocia volcanism.
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Authors
Paolo Di Giuseppe, Samuele Agostini, Piero Manetti, Mehmet Yilmaz SavaÅçın, Sandro Conticelli,