5 years ago

Fat plumes may reflect the complex rheology of the lower mantle

P. Cordier, PH. Carrez, A. Davaille
Recent tomographic imaging of the mantle below major hotspots show slow seismic velocities extending down to the core-mantle boundary, confirming the existence of mantle plumes. However, these plumes are much thicker than previously thought. Using new laboratory experiments and scaling laws, we show that thermal plumes developing in a visco-plastic fluid present much larger diameters than plumes developing in a newtonian fluid. Such a rheology requiring a yield-stress is consistent with a lower mantle predominantly deforming by pure dislocation climb. Yield stress values between 1 and 10 MPa, implying dislocation densities between 108 and 1010 m−2 would be sufficient to reproduce the plumes morphology observed in tomographic images.

Publisher URL: http://onlinelibrary.wiley.com/resolve/doi

DOI: 10.1002/2017GL076575

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