Subduction zones are dynamic regions where intense geological processes like earthquakes, volcanic eruptions, and the recycling of oceanic crust are constantly at play. A key factor that influences the behavior of these zones is *interface rheology*—the strength and viscosity of the boundary (the interface) between the subducting and overriding plates. Understanding this interface is crucial for i ...[Read More]
A New Look at the Rheology of Deep Subduction Zones
Field photos of shear zones from Syros Island, Greece. Photo credit: Ana Lorena Abila