The compensated linear‐vector dipole: A possible mechanism for deep earthquakes
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[1] L. Knopoff,et al. The mechanism at the focus of deep earthquakes , 1970 .
[2] J. Weertman. Dislocation motion on an interface with friction that is dependent on sliding velocity , 1969 .
[3] M. Randall. Relative sizes of multipolar components in deep earthquakes , 1968 .
[4] Ajit K. Mal,et al. Elastic Wave Velocities in Two-component Systems , 1967 .
[5] A. E. Ringwood,et al. The pyroxene-garnet transformation in the earth's mantle , 1967 .
[6] T. Rooney,et al. SHEAR STRENGTH, POLYMORPHISM, AND MECHANICAL BEHAVIOR OF OLIVINE, ENSTATITE, DIOPSIDE, LABRADORITE, AND PYROPE GARNET: TESTS TO 920C AND 60 KB. , 1966 .
[7] Leon Knopoff,et al. Body Force Equivalents for Seismic Dislocations , 1964 .
[8] F. Evison. Earthquakes and faults , 1963 .
[9] H. Benioff. Source wave forms of three earthquakes , 1963 .
[10] L. Knopoff,et al. First motions from seismic sources , 1960 .