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How did the Subducted Oceanic Slab Break-off Take Place?

Ji, W. Q., Wu, F. Y., Chung, S. L., et al., 2016. Eocene Neo-Tethyan Slab Breakoff Constrained by 45 Ma Oceanic Island Basalt-Type Magmatism in Southern Tibet. Geology, 44(4): 283-286. https://doi.org/10.1130/g37612.1
von Blanckenburg, F., Davies, J. H., 1995. Slab Breakoff: A Model for Syncollisional Magmatism and Tectonics in the Alps. Tectonics, 14(1): 120-131. https://doi.org/10.1029/94tc02051
Zhu, D. C., Wang, Q., Zhao, Z. D., 2017. Constraining Quantitatively the Timing and Process of Continent-Continent Collision Using Magmatic Record: Method and Examples. Science China Earth Sciences, 60(6): 1040-1056. https://doi.org/10.1007/s11430-016-9041-x