Publication Date:
2018-06-08
Description:
Slow progress is being made in quantifying the mechanical and dynamical states of the lower mantle. The large plastic strength of the mantle above the D layer exhibits a non-tidal gravity field coefficient that is driven by isostatic flow of the deep mantle, as suggested by Yoder et al.
Keywords:
Geophysics
Type:
AGU meetingon General Geophysics; San Francisco, CA; United States
Format:
text