Why does the co-seismic slip of the 1999 Chi-Chi (Taiwan) earthquake increase progressively northwestward on the plane of rupture?

Author:

Cattin R.,Loevenbruck A.,Le Pichon X.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference39 articles.

1. A review of recently active faults in Taiwan;Bonilla,1975

2. Particle motions in a physical model of shallow angle thrust faulting;Brune;Proc. Indian Acad. Sci., A Earth Planet. Sci.,1996

3. Active detachment of Taiwan illuminated by small earthquakes and its control of first-order topography;Carena;Geology,2002

4. Modeling mountain building and the seismic cycle in the Himalaya of Nepal;Cattin;J. Geophys. Res.,2000

5. Effects of superficials layers on coseismic displacements for a dip–slip fault and geophysical implications;Cattin;Geophys. J. Int.,1999

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