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Investigatingthe kinematics of mountain building in Taiwan from the spatiotemporal evolution of the foreland basin and western foothills
The kinetics of mountain building Taiwan the spatio temporal evolution of the foreland basin western foothills
2014/4/15
The Taiwanese range has resulted from the collision between the Luzon volcanic arc and the Chinese continental margin, which started about 6.5 Myr ago in the north, and has since propagated southward....
Kinematic analysis of the Pakuashan fault tip fold, west central Taiwan: Shortening rate and age of folding inception
Kinematic analysis Pakuashan fault tip fold, west central Taiwan Shortening rate age of folding inception
2014/4/15
The Pakuashan anticline is an active fault tip fold that constitutes the frontal most zone of deformation along the western piedmont of the Taiwan Range. Assessing seismic hazards associated with this...