Crs. Da Silva et al., The composition and geotherm of the lower mantle: constraints from the elasticity of silicate perovskite, PHYS E PLAN, 118(1-2), 2000, pp. 103-109
A newly developed parameterization of the third-order isentropic finite str
ain equation of states (EOS) is used in conjunction with experimental data
and theoretical results on MgSiO3 perovskite. New geotherms for the lower m
antle are derived by comparison with preliminary reference earth model (PRE
M). The geotherms are adiabatic up to 1500 km depth and super-adiabatic the
reafter. A description of the critical steps in obtaining the new parameter
ization is also given. (C) 2000 Elsevier Science B.V. All rights reserved.