1981), and at sub-crustal depths anisotropy is likely caused by arises above ~250 km. This has been linked to the dominance of dislocation vrs. diffusion creep at these depths (Karato, 1992; Gaherty and Jordan, 1995; Karato, 1998), and anisotropy may therefore constrain rheology (McNamara et al., 2002). Available online at www.sciencedirect.com Seismic shear waves that are polarized horizontally (SH), such as Love waves, travel faster on average in the upper mantle than those that are polarized vertically (SV), such as Rayleigh waves (Anderson, 1966). This observation implies a layer with radia
Abstract: The largest seismic event ever recorded on Mars, with a moment magnitude of 4.7 ±&nb...
Long-period surface waves are used to map lateral heterogeneities of velocity and anisotropy in the ...
The depth of the oceanic lithosphere–asthenosphere boundary (LAB), as inferred from shear wave veloc...
Abstract. Long-period surface waves are used to map lateral heterogenefties of velocity and anisotro...
We present a new mantle model (YB14SHani) of azimuthal anisotropy for horizontally polarized shear w...
Seismic radial anisotropy (the squared ratio between the speeds of horizontally and vertically polar...
The largest seismic event ever recorded on Mars, with a moment magnitude of 4.7 ± 0.2, is the first ...
Abstract. Rayleigh wave and Love wave dispersion data for oceanic paths cannot be satisfied by an is...
The mantle transition zone is believed to play an important role in the thermochemical evolution of ...
International audienceSurfacewave studies in the 1960s provided the first indication that the upper ...
A search for the effects of anisotropy on seismic body-waves predicted by theory is described. Prel...
Isotropic earth models are unable to provide uniform fits to the gross Earth normal mode data set or...
Summary. Anisotropy of seismic waves in the uppermost mantle has not only been observed in the ocean...
Plate formation and evolution processes are predicted to generate upper mantle seismic anisotropy an...
[1] The sensitivity of a surface wave to the lateral structure of the Earth's mantle depends on the ...
Abstract: The largest seismic event ever recorded on Mars, with a moment magnitude of 4.7 ±&nb...
Long-period surface waves are used to map lateral heterogeneities of velocity and anisotropy in the ...
The depth of the oceanic lithosphere–asthenosphere boundary (LAB), as inferred from shear wave veloc...
Abstract. Long-period surface waves are used to map lateral heterogenefties of velocity and anisotro...
We present a new mantle model (YB14SHani) of azimuthal anisotropy for horizontally polarized shear w...
Seismic radial anisotropy (the squared ratio between the speeds of horizontally and vertically polar...
The largest seismic event ever recorded on Mars, with a moment magnitude of 4.7 ± 0.2, is the first ...
Abstract. Rayleigh wave and Love wave dispersion data for oceanic paths cannot be satisfied by an is...
The mantle transition zone is believed to play an important role in the thermochemical evolution of ...
International audienceSurfacewave studies in the 1960s provided the first indication that the upper ...
A search for the effects of anisotropy on seismic body-waves predicted by theory is described. Prel...
Isotropic earth models are unable to provide uniform fits to the gross Earth normal mode data set or...
Summary. Anisotropy of seismic waves in the uppermost mantle has not only been observed in the ocean...
Plate formation and evolution processes are predicted to generate upper mantle seismic anisotropy an...
[1] The sensitivity of a surface wave to the lateral structure of the Earth's mantle depends on the ...
Abstract: The largest seismic event ever recorded on Mars, with a moment magnitude of 4.7 ±&nb...
Long-period surface waves are used to map lateral heterogeneities of velocity and anisotropy in the ...
The depth of the oceanic lithosphere–asthenosphere boundary (LAB), as inferred from shear wave veloc...