Thermochemical Mantle Convection with Drifting Deformable Continents: Main Features of Supercontinent Cycle
Author:
Funder
Russian Foundation for Basic Research
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00024-019-02164-w.pdf
Reference63 articles.
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2. Ballmer, M. D., van Hunen, J., Ito, G., Tackley, P. J., & Bianco, T. A. (2007). Non-hotspot volcano chains originating from small-scale sublithospheric convection. Geophysical Research Letters, 34, L23310. https://doi.org/10.1029/2007gl031636 .
3. Bobrov, A. M., & Baranov, A. A. (2016). The mantle convection model with non-Newtonian rheology and phase transitions: The flow structure and stress fields. Izvestiya Physics of the Solid Earth, 52(1), 129–143. https://doi.org/10.1134/s1069351316010031 .
4. Bobrov, A. M., & Baranov, A. A. (2018). Modeling of moving deformable continents by active tracers: Closing and opening of oceans, recirculation of oceanic crust. Geodynamics & Tectonophysics, 9(1), 287–307. https://doi.org/10.5800/gt-2018-9-1-0349 .
5. Bobrov, A. M., & Trubitsyn, A. P. (2008). Numerical model of the supercontinental cycle stages: integral transfer of the oceanic crust material and mantle viscous shear stresses. Studia Geophysica et Geodaetica, 52, 87–100. https://doi.org/10.1007/s11200-008-0007-1 .
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