The Sanjiang region in SE Tibet Plateau, and the western Yunnan region in southwestern
China constitute a collage of Gondwana-derived micro-continental blocks and arc terranes …

The Beiya ore deposit is located in the northwestern Yangtze Block, to the southeast of the
Tibetan Plateau, SW China. The deposit is hosted by a porphyritic monzogranitic stock that …

The lateral expansion of the southeastern Tibetan Plateau causes devastating earthquakes,
but is poorly understood. In particular, the links between regional variations in surface …

Competing geodynamic models, such as rigid-block extrusion, continuous deformation, and
the mid-lower crustal flow, have been proposed to describe the growth and expansion of …

This essential reference for graduate students and researchers provides a unified treatment
of earthquakes and faulting as two aspects of brittle tectonics at different timescales. The …

New structural, petrographic, and 40Ar/39Ar data constrain the kinematics of the ASRR
(Ailao Shan‐Red River shear zone). In the XueLong Shan (XLS), geochronological data …

The maximum-pressure Psingle bondT conditions (P max–T) and prograde Psingle bondT
paths of exhumed subduction-related metamorphic rocks are compared to predictions of …

Mechanisms for uplift and deformation of the Tibetan Plateau remain vigorously debated;
hypotheses include stepwise growth, distributed thickening, and crustal channel flow, each …

Exposures of high‐grade, midcrustal rocks within the Red River shear zone (RRSZ), which
separates the Indochina and South China blocks, exhibit clear evidence of left‐lateral …

Thermal models for Barrovian metamorphism driven by doubling the thickness of the
radiogenic crust typically meet difficulty in accounting for the observed peak metamorphic …