Subduction initiation of the Bangong–Nujiang Tethys Ocean, Tibetan Plateau
The initiation of subduction is widely recognized as a critical process associated with the
evolution of the meso-Tethys Ocean. Here, we present zircon U–Pb, Lu–Hf isotope, and …
evolution of the meso-Tethys Ocean. Here, we present zircon U–Pb, Lu–Hf isotope, and …
Detrital zircon populations of the South Qiangtang terrane, central Tibetan Plateau, and their implications for Tethyan evolution
W Xu, W Zhang, F Liu - International Geology Review, 2023 - Taylor & Francis
Detrital zircon populations of the South Qiangtang terrane (SQT) provide vital information for
reconstructing the Tethyan evolution of the Tibetan Plateau but are obscured by the …
reconstructing the Tethyan evolution of the Tibetan Plateau but are obscured by the …
Final closure of the Paleo-Tethys Ocean: Insights from Triassic granitoids in the central Qiangtang area, northern Tibetan Plateau
The geodynamic evolution during the closure of the Paleo-Tethys Ocean in the Tibetan
Plateau remains to be fully understood. The Longmu Co− Shuanghu suture zone in the …
Plateau remains to be fully understood. The Longmu Co− Shuanghu suture zone in the …
Metabasic rocks as important nitrogen carriers to forearc depths: Implications for deep nitrogen cycling
Understanding deep nitrogen (N) cycling better requires investigating the delivery of N to
subduction systems via various lithologies. Input to subduction zones through mafic rocks is …
subduction systems via various lithologies. Input to subduction zones through mafic rocks is …
Tectono-magmatic response to the geometric evolution of slab breakoff in the Paleo-Tethys Ocean: Constraints from Late Triassic granites in the Qiangtang block …
H Wu, XJ Liu, JW Chen, C Li, R Yang, ZQ Jiang - Bulletin, 2024 - pubs.geoscienceworld.org
Slab breakoff can explain the postcollisional igneous and metamorphic events in many
collisional orogens and triggers the transition from initial continental collision to deep …
collisional orogens and triggers the transition from initial continental collision to deep …