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Titlebook: Mechanics Problems in Geodynamics Part II; Part II Ren Wang,Keiiti Aki Book 1996 Birkhäuser Verlag 1996 Deformation.Geodynamik.Geophysik.Se

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Thermal Modeling of the Southern Alps, New Zealand,ay uplift rate is close to 10 mm/y. Major thermal differences between the Franz Josef and Haast profiles appear to be due to different uplift and erosion rates. There is weak evidence that frictional heating close to the Alpine fault zone is not significant. The modeling provides explanations for th
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Stress Field and Seismicity in the Indian Shield: Effects of the Collision between India and Eurasication of stresses in the upper brittle crust. Many of the faults in these linear belts, which happen to be 200–80 m.y. old, are being reactivated either in a strike-slip or thrust-faulting mode. The reactivation mechanisms have been analyzed by taking into consideration the amplification of stresse
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