Lithospheric thermal regime under the Qinling Orogenic Belt and the Weihe Basin: A transect across the Yangtze and the North China cratons in central China
Author:
Funder
National Natural Science Foundation of China
Natural Science Foundation of Shaanxi Province
China Scholarship Council
Publisher
Elsevier BV
Subject
Earth-Surface Processes,Geophysics
Reference128 articles.
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1. Different gravity anomaly, crustal structure, and uplift mechanism of the eastern and western Qinling Orogen revealed by full coverage gravimetry;Journal of Geodesy;2023-03
2. Deformation of the Qinling belt revealed byP-wave velocity and azimuthal anisotropy tomography;Geophysical Journal International;2023-02-15
3. Crustal isostatic state and lower crust delamination beneath the Qinling Orogenic Belt: Constraints from receiver function imaging;Gondwana Research;2022-03
4. Heat Flow and Thermal Source of the Xi’an Depression, Weihe Basin, Central China;Frontiers in Earth Science;2022-01-10
5. Ps-splitting analysis reveals differential crustal deformation beneath the Qinling Orogenic Belt and its surrounding areas;Geophysical Journal International;2021-12-17
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