has been cited by the following article(s):
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[1]
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Lithospheric electrical structure across the Bangong-Nujiang Suture in northern tibet revealed by magnetotelluric
Frontiers in Earth Science,
2023
DOI:10.3389/feart.2022.1085583
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[2]
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Divergent double subduction of Bangong-Nujiang Ocean revealed by high-resolution magnetotelluric data at 86°E in the northern Tibetan Plateau
Tectonophysics,
2023
DOI:10.1016/j.tecto.2023.229960
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[3]
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Electrical Response of a Reactivated Ancient Suture Revealed by Three‐Dimensional Magnetotelluric Inversion Across the Jinsha River Suture, Northern Tibetan Plateau
Journal of Geophysical Research: Solid Earth,
2023
DOI:10.1029/2022JB026264
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[4]
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Bidirectional subduction of the Bangong-Nujiang ocean revealed by deep-crustal seismic reflection profile
Tectonophysics,
2022
DOI:10.1016/j.tecto.2022.229455
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[5]
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Bidirectional subduction of the Bangong-Nujiang ocean revealed by deep-crustal seismic reflection profile
Tectonophysics,
2022
DOI:10.1016/j.tecto.2022.229455
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[6]
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Magmatic Underplating Thickening of the Crust of the Southern Tibetan Plateau Inferred From Receiver Function Analysis
Geophysical Research Letters,
2021
DOI:10.1029/2021GL093754
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[7]
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Shaping the Surface Deformation of Central and South Tibetan Plateau: Insights From Magnetotelluric Array Data
Journal of Geophysical Research: Solid Earth,
2020
DOI:10.1029/2019JB019206
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[8]
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Shaping the Surface Deformation of Central and South Tibetan Plateau: Insights From Magnetotelluric Array Data
Journal of Geophysical Research: Solid Earth,
2020
DOI:10.1029/2019JB019206
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[9]
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Lithospheric electrical structure in the central Tibetan Plateau and its tectonic significance
Journal of Asian Earth Sciences,
2019
DOI:10.1016/j.jseaes.2019.103996
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