Motif d'Images du Canada avec Comme Attributs Forme, Taille et Rotation (A)

Geotherms derived from vigorously convecting fluid mod- els of the mantle are also adiabatic provided that both in- ternal and viscous heating can be neglected, with

As shear velocity increases, the separation rate of the phases increases, demonstrating a basic feedback mechanism: Accumulation of the fluid phase causes focused weak zones

Figure 8: Unit length inferred from the 2D thermal and strength models as a function of the burial depth for: a- three different ductile crust rheologies (Wet quartz, Dry

In the Appalachians and the Pyrenees, where tele­ seismic shear-wave splitting is characterized by a fast wave dominantly parallel to the structural trend of the

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The evolution of the Baikal rift or the East African rift, for instance, probably integrates the rheological effect of the stiff Siberian or Tanzanian cratons and an anisotropy

The focus was on westward propagating signals whose phase speeds, estimated by means of the Radon Transform, appeared to be close to that anticipated for the first baroclinic mode.

[ 74 ] Soundings over Guadeloupe showing a low-level temperature inversion (indicated with cyan stripes in Figure 5) are observed on 24 June, which does not appear obviously dusty