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Dan-Ping Yan
China University of Geosciences
53Publications
22H-index
2,608Citations
Publications 53
Newest
#1Hongxu Mu (China University of Geosciences)H-Index: 2
#2Dan-Ping Yan (China University of Geosciences)H-Index: 22
Last.Shu‐Bing Li (Sinopec)H-Index: 1
view all 7 authors...
Abstract The Upper Triassic Xujiahe Formation is a succession of continental clastic rocks in the western Sichuan Basin, China. This formation has previously been regarded as deposited in a foreland basin linked to the NE-SW-striking Longmen Shan Thrust Belt. However, this hypothesis is questionable due to the presence of faults within the Longmen Shan Thrust Belt. Focusing on the Late Triassic proto-basin, we obtained new data from both outcrops and boreholes, which provide information on the s...
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#1Liang Qiu (China University of Geosciences)H-Index: 1
#2Dan-Ping Yan (China University of Geosciences)H-Index: 22
Last.Yixi Zhang (China University of Geosciences)H-Index: 3
view all 6 authors...
The 1500-km-long Jiangnan tectonic belt in China is well known for large outcrops of Proterozoic basement rocks, although the exhumation history of the exposed basement is poorly constrained. This study performed thermochronology of the Sanfang batholith in the southernmost section of this belt to constrain the timing and mechanism of exhumation. Granite samples collected along three transects were subjected to apatite fission-track analysis. The results show that the ages of single apatite grai...
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#1Ruoyan Kong (China University of Geosciences)H-Index: 1
#2Dan-Ping Yan (China University of Geosciences)H-Index: 22
Last.Ling-Xiao Gong (China University of Geosciences)
view all 8 authors...
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#1Liang Qiu (China University of Geosciences)H-Index: 5
#2Wen-Xin Yang (China University of Geosciences)H-Index: 3
Last.Fang-Yue Wang (Hefei University of Technology)
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Two phases of diabase-sill-forming magmatism are recorded within the Badu anticline where magmas were emplaced into upper Palaeozoic carbonates and clastic rocks of the Youjiang fold-and-thrust belt in the SW South China Block, China. Zircons from these diabase units yield weighted mean U–Pb ages of 249.2±2.0 Ma and 187.1±3.3 Ma, and magmatic oxygen fugacity values from ‒20 to ‒6 (average of ‒12, equating to FMQ +5) and ‒20 to ‒10 (average of ‒15, equating to FMQ +2), respectively. These data in...
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#1Dan-Ping Yan (China University of Geosciences)H-Index: 22
#2Liang Qiu (China University of Geosciences)H-Index: 2
Last.Shu‐Bing Li (Sinopec)H-Index: 1
view all 9 authors...
6 CitationsSource
#1Liang Qiu (China University of Geosciences)H-Index: 5
#2Ruoyan Kong (China University of Geosciences)H-Index: 1
Last.Shahnawaz Ariser (China University of Geosciences)H-Index: 2
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Abstract Liaodong Peninsula on the northeastern North China Block that witnessed the spectacular Late Mesozoic tectonics is a key area to probe the transition from compression to extension. Borehole data clearly reveals that the Cambrian limestone overlay the Jurassic limestone, which identified the Yuantai thrust system in Liaodong Peninsula. Zircon grains from a granodiorite dike that intruded the thrust system yielded U-Pb age of 128.3 ± 1.3 Ma, further constraining the timing of the thrustin...
5 CitationsSource
#1Dan-Ping Yan (China University of Geosciences)H-Index: 22
#2Yu Zhou (China University of Geosciences)H-Index: 1
Last.Chen-Guang Xu (China University of Geosciences)H-Index: 1
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Abstract The Longmenshan Tectonic Complex (LSTC), along the eastern margin of the Tibetan Plateau, the site of devastating earthquakes such as the magnitude 8.0 (Wenchuan) earthquake on 12 May 2008, preserves an exceptionally complete history of the tectonic evolution of the Yangtze block and its relations to adjacent tectonic units. Due to sequential tectonic superposition and tectonic reactivation, the tectonic nature of the LSTC, and in particularly the older history, has been profoundly deba...
22 CitationsSource
#1Ming Sun (China University of Geosciences)H-Index: 2
#2An Yin (China University of Geosciences)H-Index: 63
Last.Liang Qiu (China University of Geosciences)H-Index: 1
view all 7 authors...
Abstract Pre-existing weakness due to repeated tectonic, metamorphic, and magmatic events is a fundamental feature of the continental lithosphere on Earth. Because of this, continental deformation results from a combined effect of boundary conditions imposed by plate tectonic processes and heterogeneous and anisotropic mechanical strength inherited from protracted continental evolution. In this study, we assess how this interaction may have controlled the Cenozoic evolution of the eastern Tibeta...
12 CitationsSource
#1Han Xu (China University of Geosciences)H-Index: 1
#2Xin-Wen Wang (China University of Geosciences)H-Index: 1
Last.Liang Qiu (China University of Geosciences)H-Index: 5
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Abstract The Dongpu Sag, located in the Bohai Bay Basin, NE China, is a Cenozoic continental rift basin. The post-rift evolution of the Dongpu Sag is associated with the development of petroleum reservoirs and has implications for Neogene–Quaternary basin evolution along the eastern margin of Eurasia. To determine the nature and origin of post-rift subsidence in the Dongpu Sag, we apply backstripping, modified strain-rate inversion, and revised finite extension modelling techniques, using data f...
3 CitationsSource
#1Liang Qiu (China University of Geosciences)H-Index: 5
#2Dan-Ping Yan (China University of Geosciences)H-Index: 22
Last.Yong-Wen Wang (China University of Geosciences)H-Index: 1
view all 10 authors...
Abstract Uranium deposits are diverse as a result of their formation in a wide variety of geological environments. However, the source of the uranium within these deposits is difficult to identify and as a result it is usually poorly understood. This study focuses on the hydrothermal Sanqiliu and Sanqisi uranium deposits, both of which formed within NE–SW striking shear zones that cross-cut the Sanfang batholith and low-grade metasedimentary rocks of the Motianling district, southern China. The ...
3 CitationsSource
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