Rheological Weakening of Subducted Slabs Due to the Persistence of Metastable Olivine Down to 600 Km Depth

Riedel, M. R., & Karato, S. (1997). Rheological Weakening of Subducted Slabs Due to the Persistence of Metastable Olivine Down to 600 Km Depth. In Upper Mantle Heterogeneities from Active and Passive Seismology (pp. 325–332). Springer Netherlands. https://doi.org/10.1007/978-94-015-8979-6_32