The tectonic evolution of the Indian plate, which started in Late Jurassic about 167million
years ago (~ 167Ma) with the breakup of Gondwana, presents an exceptional and intricate …

Using the most up-to-the-date information available, we present a considerably revised plate
tectonic and paleogeographic model for the Indian Ocean bordering continents, from …

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 …

Research by many workers in various regions of the Himalaya, combined with our recent
geologic and geochronologic studies in Nepal, indicate that fundamental aspects of the …

Original stable isotope compositions of carbonates representing conditions in the latest
Oligocene-early Miocene Kailas and Qiabulin areas, both in southern Tibet, record …

The Himalaya consists of thrust sheets tectonically shingled together since~ 58 Ma as India
collided with and slid beneath Asia. Major Himalayan structures, including the South Tibetan …

The India–Asia collision resulted in the construction of the vast Himalayan orogen. The
northern Himalayan domain began to experience extensional tectonics since Eocene …

A central debate for the evolution of the Himalayan orogen is how the Greater Himalayan
Crystalline complex in its core was emplaced during the Cenozoic Indo-Asian collision …

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Stratigraphic and petrographic analysis of the Cretaceous to Eocene Tibetan sedimentary
succession has allowed us to reinterpret in detail the sequence of events which led to …