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A new growth model of the northeastern Tibetan Plateau from high-resolution seismic imaging by improved double-difference tomography [期刊论文]
Tectonophysics, 2021-01-01, 798
Sun Q.;  Pei S.;  Cui Z.;  Chen Y.J.;  Liu Y.;  Xue X.;  Li J.;  Li L.;  Zuo H.
View/Download:10/0
 
An immediate response to the Indian-Eurasian collision along the northeastern Tibetan Plateau: Evidence from apatite fission track analysis in the Kuantan Shan-Hei Shan [期刊论文]
Tectonophysics, 2020-01-01, 774
An K.;  Lin X.;  Wu L.;  Yang R.;  Chen H.;  Cheng X.;  Xia Q.;  Zhang F.;  Ding W.;  Gao S.;  Li C.;  Zhang Y.
View/Download:0/0
 
Diachronous uplift in intra-continental orogeny: 2D thermo-mechanical modeling of the India-Asia collision [期刊论文]
Tectonophysics, 2020-01-01, 775
Bian S.;  Gong J.;  Chen L.;  Zuza A.V.;  Chen H.;  Lin X.;  Cheng X.;  Yang R.
View/Download:5/0
 
Provenance analysis of Cretaceous peripheral foreland basin in central Tibet: Implications to precise timing on the initial Lhasa-Qiangtang collision [期刊论文]
Tectonophysics, 2020-01-01, 775
Chen Y.;  Ding L.;  Li Z.;  Laskowski A.K.;  Li J.;  Baral U.;  Qasim M.;  Yue Y.
View/Download:0/0
 
Significance of crustal extension and magmatism to gold deposits beneath Jiaodong Peninsula, eastern North China Craton: Seismic evidence from receiver function imaging with a dense array [期刊论文]
Tectonophysics, 2020-01-01, 789
Yu G.;  Xu T.;  Ai Y.;  Chen L.;  Yang J.
View/Download:7/0
 
Structural architecture and tectonic evolution of the Cenozoic Zhanhua Sag along the Tan–Lu Fault Zone in the eastern North China: Reconciliation of tectonic models on the origin of the Bohai Bay Basin [期刊论文]
Tectonophysics, 2020-01-01, 775
Zhang Y.;  Dilek Y.;  Zhang F.-Q.;  Chen H.-L.;  Zhu C.-T.;  Hao X.-F.
View/Download:0/0
 
High resolution crustal model of SE Tibet from joint inversion of seismic P-wave travel-times and Bouguer gravity anomalies and its implication for the crustal channel flow [期刊论文]
Tectonophysics, 2020-01-01, 792
Zhao Y.;  Guo L.;  Guo Z.;  Chen Y.J.;  Shi L.;  Li Y.
View/Download:3/0
 

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