Apatite Geo-Thermochronology and Geochemistry Constrain Oligocene-Miocene Growth and Geodynamics of the Northeastern Tibetan Plateau

Autor(en)
Chao Guo, Zhiyong Zhang, Richard Lease, Marco G. Malusà, David Chew, Haijian Lu, Lin Wu, Dunfeng Xiang, Nan Wang, Bernhard Grasemann, Wenjiao Xiao
Abstrakt

Understanding the geodynamics of plateau evolution requires examining the spatial and temporal aspects of mountain building in the northeastern Tibetan Plateau, which are still under debate. Here we integrate apatite geo-thermochronological and geochemical data from the Oligocene-Miocene succession of the Xunhua Basin to elucidate the evolution of the regional topography. The results suggest sediment provenance changes, at ca. 28, 20 and 12 Ma, indicating topographic growth of the West Qinling, Laji Shan, and Jishi Shan source areas, respectively. Our findings reveal Oligocene-Miocene stepwise deformation and middle Miocene stress reorganization within the northeastern Tibetan Plateau. We attribute this to Oligocene lithospheric foundering beneath the south-central Tibetan Plateau and the middle Miocene initiation of sinistral strike-slip faults due to the underthrusting of India and North China. This study highlights the roles of lithospheric removal and continental underthrusting in plateau growth, and the value of multi-proxy apatite analyses in provenance studies.

Organisation(en)
Institut für Geologie
Externe Organisation(en)
Chinese Academy of Sciences (CAS), United States Geological Survey, Università degli Studi di Milano-Bicocca, University of Dublin, Chinese Academy of Geological Sciences
Journal
Geophysical Research Letters
Band
52
ISSN
0094-8276
DOI
https://doi.org/10.1029/2024GL113157
Publikationsdatum
02-2025
Peer-reviewed
Ja
ÖFOS 2012
105124 Tektonik
Schlagwörter
ASJC Scopus Sachgebiete
Geophysics, Allgemeine Erdkunde und Planetologie
Link zum Portal
https://ucrisportal.univie.ac.at/de/publications/732aeec7-6125-43bb-9155-92d64b173b13