The subduction plate interface is continuously shaped by mass and fluid transport along and across it, in an ever increasing pressure-temperature-strain regime, that influence crucially the seismicity, magmatism, and element re-distribution along convergent margins. The session aims to put toghether contributions dealing with fossil or active subduction zones and integrating results from structural geology, petrology/geochemistry, and modelling, in an attempt to decipher the processes active along the subduction plate interface from the surface down to ca. 100 km.
Invited speaker: Michele Zucali (UNIMI)
Francesca, Francesca & Laura