D-Rex, a program for calculation of seismic anisotropy due to crystal lattice preferred orientation in the convective upper mantle

E Kaminski, NM Ribe… - Geophysical Journal …, 2004 - academic.oup.com
Models of development of lattice preferred orientation (LPO) of crystals aggregates in
convective flow are necessary to interpret the anisotropic seismic signature of the Earth′ s …
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[引用][C] D-Rex, a program for calculation of seismic anisotropy due to crystal lattice preferred orientation in the convective upper mantle

É Kaminski, NM Ribe, JT Browaeys - Geophysical Journal International, 2004 - cir.nii.ac.jp
D-Rex, a program for calculation of seismic anisotropy due to crystal lattice preferred orientation
in the convective upper mantle | CiNii Research CiNii 国立情報学研究所 学術情報ナビゲータ …

D-Rex, a program for calculation of seismic anisotropy due to crystal lattice preferred orientation in the convective upper mantle

É Kaminski, NM Ribe… - Geophysical Journal …, 2004 - ieeexplore.ieee.org
Models of development of lattice preferred orientation (LPO) of crystals aggregates in
convective flow are necessary to interpret the anisotropic seismic signature of the Earth′ s …
[PDF] ipgp.fr

[PDF][PDF] D-Rex, a program for calculation of seismic anisotropy due to crystal lattice preferred orientation in the convective upper mantle

E Kaminski, NM Ribe, JT Browaeys - Geophys. J. Int, 2004 - ipgp.fr
Models of development of lattice preferred orientation (LPO) of crystals aggregates in
convective flow are necessary to interpret the anisotropic seismic signature of the Earth's …

D-Rex, a program for calculation of seismic anisotropy due to crystal lattice preferred orientation in the convective upper mantle

E Kaminski, NM Ribe, JT Browaeys - Geophysical Journal International, 2004 - elibrary.ru
Models of development of lattice preferred orientation (LPO) of crystals aggregates in
convective flow are necessary to interpret the anisotropic seismic signature of the Earth's …
[HTML] harvard.edu

[HTML][HTML] D-Rex, a program for calculation of seismic anisotropy due to crystal lattice preferred orientation in the convective upper mantle

É Kaminski, NM Ribe… - … 158, Issue 2, pp. 744-752., 2004 - adsabs.harvard.edu
Abstract Models of development of lattice preferred orientation (LPO) of crystals aggregates
in convective flow are necessary to interpret the anisotropic seismic signature of the Earth's …

D-REX, A PROGRAM FOR CALCULATION OF SEISMIC ANISOTROPY DUE TO CRYSTAL LATTICE PREFERRED ORIENTATION IN THE CONVECTIVE UPPER …

E Kaminski, NM Ribe - 2004 - repository.geologyscience.ru
Models of development of lattice preferred orientation (LPO) of crystals aggregates in
convective flow are necessary to interpret the anisotropic seismic signature of the Earth's …
[PDF] academia.edu

[PDF][PDF] D-Rex, a program for calculation of seismic anisotropy due to crystal lattice preferred orientation in the convective upper mantle

E Kaminski, NM Ribe, JT Browaeys - Geophys. J. Int, 2004 - academia.edu
Models of development of lattice preferred orientation (LPO) of crystals aggregates in
convective flow are necessary to interpret the anisotropic seismic signature of the Earth's …

D‐Rex, a program for calculation of seismic anisotropy due to crystal lattice preferred orientation in the convective upper mantle

É Kaminski, NM Ribe… - Geophysical Journal …, 2004 - Wiley Online Library
Models of development of lattice preferred orientation (LPO) of crystals aggregates in
convective flow are necessary to interpret the anisotropic seismic signature of the Earth's …