A review of the geologic history of the Himalayan-Tibetan orogen suggests that at least 1400
km of north-south shortening has been absorbed by the orogen since the onset of the Indo …

Crustal shortening and thickening to c. 70–85 km in the Tibetan Plateau occurred both
before and mainly after the c. 50 Ma India–Asia collision. Potassic–ultrapotassic shoshonitic …

We process rigorously GPS data observed during the past 25 years from continental China
to derive site secular velocities. Analysis of the velocity solution leads to the following …

Global Positioning System (GPS) measurements in China indicate that crustal shortening
accommodates most of India's penetration into Eurasia. Deformation within the Tibetan …

We derive a detailed horizontal velocity field for the southeast borderland of the Tibetan
Plateau using GPS data collected from the Crustal Motion Observation Network of China …

The active left-slip Altyn Tagh fault defines the northern edge of the Tibetan plateau. To
determine its deformation history we conducted integrated research on Cenozoic …

We present a new global model for Recent plate velocities, REVEL, describing the relative
velocities of 19 plates and continental blocks. The model is derived from publicly available …

In this paper we present a global model (GSRM-1) of both horizontal velocities on the Earth's
surface and horizontal strain rates for almost all deforming plate boundary zones. A model …

On the basis of a synthesis of tectonic data available on the India‐Asia collision, we present
a first attempt to reconstruct the evolution of the collision zone. Assuming that the …

Studies of Late Quaternary geological slip-rates and the GPS decadal slip-rates along the
major strike-slip faults in the northern margin of the Tibetan Plateau show that slip-rates …