The crustal shortening /thickening within high Tibet and its tectonic ...

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Velocity Pattern for Viscous medium 1 Distributed deformation throughout crust 2 Velocity changes little across active fault 3 Smooth velocity curve, decrease monotonically or linearly with respect to fixed point Visco-elastic Medium Driving Force Velocity fault Fixed point O Length Continuously Deforming Extension GPS Profile across boundary zone between the Australian and Pacific Plate, New Zealand, Bourne et al, Nature, 391, 655,1998
GPS across Tibetan Plateau Conclusion I : In general, Conclusion GPS across I : Tibet shows a linearly In general, GPS across decreased velocity rates Tibet shows a linearly respect to Siberia from decreased velocity rates 40 mm/yr to zero respect to Siberia from 40 mm/yr to zero Wang et al. Science, 249, 574, 2001 Conclusion II : Faults in Tibet slip at rates no more than 10 mm/yr except Himalayas, Perhaps the deformation is continuous and homogeneous Zhang et al., Geology,32, 809, 2004 Problem : Sparse dataset does not rule out the discontinuous mode
Page 1 and 2: Hotine-Marussi Symposium of Theoret
Page 3 and 4: Telling Feature : Raised Tibet with
Page 5 and 6: Uplift mode in Tibet II Indentor (
Page 7 and 8: Approaches for Model Constraint 1 T
Page 9: Velocity Pattern for rigid blocks :
Page 14 and 15: GPS Profile across Tibet mm/yr Zanb
Page 16 and 17: Fault Plane Solution of Earthquake
Page 18 and 19: Summary • New GPS show a pattern
Page 20: Hotine-Marussi Symposium of Theoret

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