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Crust-mantle decoupling

Brown, C. D. Phillips, R. J. 2000. Crust-mantle decoupling by flexure of continental lithosphere. Journal of Geophysical Research, 105(B6), 13 221-13237. [Pg.208]

Isotope decoupling between oceanic mantle and crust evidence for marble-cake or veined mantle 156... [Pg.805]

An important interpretation of observed anisotropy centres on whether or not the crust is coupled to the mantle during orogenic episodes (Silver 1996). Silver and coworkers (Silver Chan 1988 Savage Silver 1993) referred to the coupled case as vertically coherent deformation (VCD) and the decoupled case as simple astheno-spheric flow (SAP). In the VCD case it is arped that anisotropy will be frozen into the lithosphere at the time of deformation and the orientation of the anisotropy will mimic trends in the surface geology. In contrast, Vinnik and coworkers have argued that in the SAP case the orientation of the anisotropy will reflect absolute plate motions (Vinnik et al. 1992). Analysis of... [Pg.33]

Royden, L. 1996. Coupling and decoupling of crust and mantle in convergent orogens implications for strain partitioning in the crust. Journal of Geophysical Research, B Solid Earth and Planets, 101, 17679-17705. [Pg.179]

See other pages where Crust-mantle decoupling is mentioned: [Pg.207]    [Pg.207]    [Pg.207]    [Pg.207]    [Pg.817]    [Pg.859]    [Pg.4410]    [Pg.115]    [Pg.157]    [Pg.230]    [Pg.278]    [Pg.280]    [Pg.10]    [Pg.20]    [Pg.20]    [Pg.858]    [Pg.858]    [Pg.136]    [Pg.188]    [Pg.156]    [Pg.156]    [Pg.254]    [Pg.18]    [Pg.283]    [Pg.74]   
See also in sourсe #XX -- [ Pg.207 ]



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