Layered convection with an interface at a depth of 1000km: stability and generation of slab-like downwellings
Author:
Publisher
Elsevier BV
Subject
Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics
Cited by 8 articles. 订阅此论文施引文献 订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献
1. Density and viscosity changes between depleted and primordial mantle at ∼1000 km depth influence plume upwelling behavior;Earth and Planetary Science Letters;2021-12
2. Effective buoyancy ratio: a new parameter for characterizing thermo-chemical mixing in the Earth's mantle;Solid Earth;2015-01-28
3. Effective buoyancy ratio: a new parameter to characterize thermo-chemical mixing in the Earth's mantle;2014-09-01
4. The fate of the slabs interacting with a density/viscosity hill in the mid-mantle;Physics of the Earth and Planetary Interiors;2010-06
5. Deep-level geodynamics: boundaries of the process according to geochemic and petrologic data;Geodynamics & Tectonophysics;2010
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