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 …

Reconstructing the evolution of the Bangong-Nujiang Tethyan Ocean (BNTO) plays an
indispensable role in understanding the linkage between Gondwana dispersion and Tibetan …

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 …

Paleoelevation reconstruction using oxygen isotopes is making a significant contribution to
understanding the Cenozoic uplift of the Himalayas and the Tibetan Plateau. This paper …

The southern Qiangtang magmatic belt was formed by the north-dipping subduction of the
Bangong–Nujiang Tethyan Ocean during Mesozoic. To better understand the petrogenesis …

We report geochronologic, whole‐rock geochemical and Sr–Nd isotopic analyses of the
granites that are exposed to both the north and the inside of the Bangong–Nujiang Suture …

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 Mesozoic strata, within the Bangong-Nujiang suture zone in central Tibet, recorded
critical information about the subduction-accretion processes of the Bangong-Nujiang …

Constraining the growth of the Tibetan Plateau in time and space is critical for testing
geodynamic models and climatic changes at the regional and global scale. The Lhasa block …

The subduction polarity and related arc–magmatic evolutional history of the Bangong–
Nujiang Ocean, which separated the South Qiangtang terrane to the north from the North …