The continental crust in the overriding plate of the India-Asia collision zone in southern Tibet
is characterized by an overthickened layer of felsic composition with an underlying granulite …

The vast eastern-Tethyan oceanic domain that throughout the Mesozoic extended between
Gondwana and Eurasia was a puzzle of larger and smaller microcontinents separated by …

Abstract The Neo-Tethys Ocean was an eastward-ga** triangular oceanic embayment
between Laurasia to the north and Gondwana to the south. The Neo-Tethys Ocean was …

The Tethyan metallogenic domain (TMD), as one of the three major domains in the world,
extends over 10000 km from east to west, and has developed several world-class …

Abstract Knowledge of the timing of the closure of the Meso-Tethys Ocean as represented by
the Bangong–Nujiang Suture Zone, ie, the timing of the Lhasa-Qiangtang collision, is critical …

The Jurassic subduction of the Bangong-Nujiang Tethys Ocean is recognized as a
significant event in the geotectonic evolution of Tibetan Plateau. This study focuses on the …

The detrital zircon has been most widely used in sediment provenance studies and basin
analysis over the past 20 years. With the accumulation of a bounty of detrital zircon ages …

Timing of the opening of the Meso-Tethys Ocean, represented by the Bangong–Nujiang
Suture Zone on the Tibetan Plateau, remains controversial. Further research is required to …

The temporal and spatial variations of exhumation in the central Tibetan Plateau (TP)
contain information about timing of the initial rise and growth of the TP. Here, we present …

Abstract The Bangong‐Nujiang Suture Zone (BNSZ) in central Tibet represents relics of the
Meso‐Tethys Ocean that once separated the Lhasa and Qiangtang terranes. When and how …