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Deformation mode of talc from subsurface to dehydration conditions: implications for the subducting oceanic lithosphere
Deformation mode of talc from subsurface to dehydration conditions: implications for the subducting oceanic lithosphere
2006
Muriel Andreani
J. Escartin
Gerhard A. Hirth
B. A. Evans
Keywords:
Talc
Shear zone
Lithosphere
Strain rate
Geophysics
van der Waals force
Deformation (mechanics)
Geology
Correction
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