The two most recent eruptive events of Nisyros volcano (Greece) record the interaction between variably evolved magmas by the presence of mafic enclaves, indicative of multiple recharge events within the magma chamber. We use the mineral chemistry composition to constrain the location of the main eruptible reservoirs and their evolution at the transition from explosive to effusive activities, with implications for magma migration and storage in the crust.


Reference

Eleonora Braschi, Francesca Giannetti, Filippo Mastroianni, Andrea Orlando, Riccardo Avanzinelli, Simone Tommasini, Georges Enea Vougioukalakis, and Lorella Francalanci, 2025. Changing magma dynamics and plumbing system architecture at an explosive–effusive transition: the case of Nisyros volcano (Greece). Eur. J. Mineral., 37, 793–817, 2025 https://doi.org/10.5194/ejm-37-793-2025

For further information: Eleonora Braschi - eleonora.braschi@cnr.it