We study internal deformation of the Taiwan orogen, a young arc-continental collision belt,
which the spatial heterogeneity remains unclear. We aim to ascertain heterogeneity of the …

Rock uplift on the Earth surface is a key observation for studies of tectonics and geodynamic
processes. Geodetic measurements from Global Positioning System (GPS) and leveling are …

Paleostress inversion of 141 outcrop-scale faults across the eastern flank of the southern
Central Range of Taiwan where leveling and GPS data suggest a steep gradient in rock …

Recently discovered numerous mud volcanoes (MVs) and mud diapirs (MDs) in SW Taiwan,
both onshore and offshore, show eruption lineaments suspected to be related to neotectonic …

Southwest (SW) Taiwan lies on the deformation front of a plate collision zone. Most
earthquakes in this region occur due to deformation of the upper crust, therefore, potential …

Southwestern Taiwan exhibits multiple fold-thrust systems as a consequence of the
interaction between the Philippine Sea Plate and the Eurasian Plate. A prominent geological …

Deep postseismic slips that reflect the rheology and the deformation of the seismogenic fault
after large earthquakes are usually investigated less than shallow slips because of the …

Taiwan is located at the boundary between the Philippine Sea plate and the passive
continental margin of the Eurasian plate and is one of the most seismically active regions in …

The paper makes a novel attempt to present a mathematical model for a buried source in the
homogeneous reduced micropolar half-space and to study the propagation of waves when …

Abstract Knowledge of what governs the interaction between slow‐and fast‐slip
earthquakes is essential to understanding the nature of the earthquake cycle. In southern …