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 …

Recent studies in the Yardoi gneiss dome of the Tethyan Himalaya, southern Tibet
demonstrated that the Himalayan orogenic belt experienced a major episode of crustal …

A Tarim to Indus traverse provides insight into the tectonics of western Tibet. The Kunlun
was the site of a Mid-Paleozoic collision. At least three phases of post-Paleozoic accretion …

The Himalayan-Tibetan orogen culminated during the Cenozoic India--Asia collision, but its
geological framework and initial growth were fundamentally the result of multiple, previous …

Cenozoic magmatism on the Tibetan plateau shows systematic variations in space and time
that must be considered in models concerning Tibetan tectonic evolution. After the India …

Long-standing problems in the geological evolution of the Tibetan–Himalayan orogen
include where the India–Asia convergence was accommodated and how the plateau grew …

The Lhasa terrane in southern Tibet is composed of Precambrian crystalline basement,
Paleozoic to Mesozoic sedimentary strata and Paleozoic to Cenozoic magmatic rocks. This …

In the Shiquanhe area of far‐western Tibet, mid‐Cretaceous strata lie unconformable on
ophiolitic melange and Jurassic flysch associated with the Bangong‐Nujiang suture zone …

Abstract Uplift of the Tibetan Plateau is thought to be one of the most important orogenic and
climate forcing events of the Cenozoic Era, associated with geodynamic changes related to …

The stable isotope composition of pedogenic and early diagenetic carbonates from the
Oiyug Basin of southern Tibet allows model estimates of the paleoaltimetry of the Tibetan …