Referencing of Continental‐Scale InSAR‐Derived Velocity Fields: Case Study of the Eastern Tibetan Plateau

Abstract

The ever-increasing temporal resolution and spatial coverage of radar interferometry (InSAR) satellite data has expanded the application fields of InSAR. For tectonic studies of active faulting and continental-scale deformation, the use of InSAR has gradually evolved from local-scale studies of earthquakes and fault seismic cycle (e.g., Bürgmann et al., 2000;Massonnet et al., 1993) to analyzes at the large-scale of major fault systems and plate-tectonics (e.g.,