H__RSES_CLINTON_Clinton

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Papers dealing with seismic anisotropy
[Savage, 1999, Silver, 1996]
Barruol, G. and Mainprice, D. (1993), A quantitative evaluation of the contribution of crustal
rocks to the shear wave splitting of teleseismic SKS waves, Physics of the Earth and
Planetary Interiors 78(3-4), 281-300.
Barruol, G., Silver, P.G. and Vauchez, A. (1997), Seismic anisotropy in the eastern United
States : deep structure of a complex continental plate, Journal of Geophysical
Research 102(B4), 8329-8348.
Barruol, G., Souriau, A., Vauchez, A., Diaz, J., Gallart, J., Tubia, J. and Cuevas, J. (1998),
Lithospheric anisotropy beneath the Pyrenees from shear wave splitting, Journal of
Geophysical Research 103(B12), 30039-30053.
Bormann, P., Gruenthal, G., Kind, R. and Montag, H. (1996), Upper mantle anisotropy
beneath Central Europe from SKS wave splitting : effects of absolute plate motion and
lithosphere-asthenosphere boundary topography ?, Journal of Geodynamics 22(1-2),
11-32.
Bowman, J.R. and Ando, M. (1987), Shear-wave splitting in the upper-mantle wedge above
the Tonga subduction zone, Geophysical Journal of the Royal Astronomical Society
8(1), 25-41.
Heintz, M., Vauchez, A., Assumpção, M., Barruol, G. and Egydio-Silva, M. (2003), Shear
wave splitting in SE Brazil : an effect of active or fossil upper mantle flow, or both,
Earth and Planetary Science Letters 211, 79-95.
Herquel, G., Wittlinger, G. and Guilbert, J. (1995), Anisotropy and crustal thickness of
Northern-Tibet. New constraints for tectonic modelling, Geophysical Research Letters
22(14), 1925-1928.
James, D.E. and Assumpção, M. (1996), Tectonic implications of S-wave anisotropy beneath
SE Brazil, Geophysical Journal International 126, 1-10.
Kendall, J.M. and Silver, P.G. (1998), Investigating causes of D'' anisotropy, Geodynamics
Series 28, 97-118.
Mainprice, D., Barruol, G. and Ben Ismail, W. (2000), The seismic anisotropy of the Earth's
mantle : from single crystal to polycrystal, Geophysical Monograph 117, 237-264.
McNamara, D.E., Owens, T.J., Silver, P.G. and Wu, F.T. (1994), Shear wave anisotropy
beneath the Tibetan Plateau, Journal of Geophysical Research 99(B7), 13655-13665.
Menke, W. and Levin, V. (2003), The cross-convolution method for interpreting SKS splitting
observations, with application to one and two layer anisotropic Earth models,
Geophysical Journal International 154(2), 379-392.
Savage, M.K. (1999), Seismic anisotropy and mantle deformation : what have we learned
from shear wave splitting ?, Reviews of Geophysics 37(1), 65-106.
Silver, P.G. (1996), Seismic anisotropy beneath the continents : probing the depths of
Geology, Annual Review of Earth and Planetary Sciences 24, 385-432.
Silver, P.G. and Chan, W.W. (1991), Shear wave splitting and subcontinental mantle
deformation, Journal of Geophysical Research 96(B10), 16429-16454.
Vauchez, A. and Nicolas, A. (1991), Mountain-building : strike-parallel motion and mantle
anisotropy, Tectonophysics 185(3-4), 183-201.
Vinnik, L.P., Makeyeva, L.I., Milev, A. and Usenko, A.Y. (1992), Golbal patterns of
azimuthal anisotropy and deformations in the continental mantle, Geophysical Journal
International 111(3), 433-447.
Wolfe, C.J. and Silver, P.G. (1998), Seismic anisotropy of oceanic upper mantle : shear wave
splitting methodologies and observations, Journal of Geophysical Research 103(1),
749-771.
Wookey, J., Kendall, J.M. and Barruol, G. (2002), Mid-mantle deformation inferred from
seismic anisotropy, Nature 415(6873), 777-780.
Causes of seismic anisotropy
[Mainprice, et al., 2000, Vinnik, et al., 1992]
Absolute plate motion related anisotropy
[Bormann, et al., 1996, Vinnik, et al., 1992]
Frozen-in anisotropy related to the last tectonic event
[Barruol, et al., 1997, Barruol, et al., 1998, James and Assumpção, 1996, Vauchez and
Nicolas, 1991]
[Heintz, et al., 2003]
Contribution to the splitting measured at the surface :
D’’ layer
[Kendall and Silver, 1998]
Lower mantle
[Wookey, et al., 2002]
Crust
[Barruol and Mainprice, 1993, Herquel, et al., 1995, McNamara, et al.,
1994]
Methodology : the most commonly used algorithm is the one developed by Silver and Chan
[Silver and Chan, 1991] together with the multiple-event method of Wolfe and Silver [Wolfe
and Silver, 1998]
A few other methods exist, as the cross-correlation (Bowman and Ando [Bowman and Ando,
1987] developed a method based on the maximal similarity in the pulse shapes of the two
rotated seismogram components) and the cross-convolution [Menke and Levin, 2003] one.
An other algorithm has been developed by Ivan Marian. Comparing results obtained by
performing two different methods (his, and the cross-convolution one) on data recorded at the
PSZ Hungarian station (GEOFON network) he found slight differences in the orientation of
the polarisation plane of the fast S-wave and in the delay times.
His codes are available through the ORFEUS system
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