作者: Jesse Wimert , Saswata Hier-Majumder
DOI: 10.1029/2011JB009012
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摘要: [1] This article presents a three-dimensional microgeodynamic model of grain-melt geometry in partially molten rocks. The isotropic unit cell the rock is characterized by face-centered-cubic symmetry, consisting rhombic dodecahedral grains. variation surface tension between grain-grain and contacts excites coupled viscous flow within grains interstitial melt, leading to steady state geometry. We obtain fractional area intergranular contact, contiguity, from these models as function melt volume fraction, fractions 0.05 0.25. Comparison with previous results indicates that contiguity lower than two-dimensional models. contrast two- values increases at high fractions. apply our ultralow-velocity zones (ULVZs) very low velocity province (VLVP) Earth's core-mantle boundary. observed seismic signature ULVZ VLVP can be explained peridotite 0.08 0.12 0.01 0.05, respectively, matrix elastic properties similar Preliminary Earth Reference Model.