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 …

The formation of the Cenozoic NS striking rifts in the Tibetan Plateau is the consequence of
continuous contraction after the India-Asia collision. Its formation and evolution are of great …

A database containing previously published geochronologic, geochemical, and isotopic
data on Mesozoic to Quaternary igneous rocks in the Himalayan‐Tibetan orogenic system …

Abstract The Tibetan Plateau is undergoing eastward extension on north-trending rifts, but
the cause is unclear. The extension is commonly thought to represent gravitational collapse …

Lithium (Li), a crucial mineral resource for modern high-tech industries, is notably abundant
in the northern Tibetan Plateau, primarily within lithium-rich salt lakes. However, the …