Flat-slab segments are considered refrigerated areas given that the asthenospheric wedge is forced to shift hundreds of kilometres away from the trench, and the flat and coupled subducting plate acts as a thermal insulator. Although lithospheric-scale thermal...
CITATION STYLE
Collo, G., Ezpeleta, M., Dávila, F. M., Giménez, M., Soler, S., Martina, F., … Schiuma, M. (2018). Basin Thermal Structure in the Chilean-Pampean Flat Subduction Zone (pp. 537–564). https://doi.org/10.1007/978-3-319-67774-3_21
Mendeley helps you to discover research relevant for your work.