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Shaocheng Ji

Affiliations: 
Civil Engineering, Geology, and Mining Ecole Polytechnique, Montreal (Canada) 
Area:
Geophysical Engineering, Geological Engineering
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"Shaocheng Ji"
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Shengsi Sun grad student 2012 Ecole Polytechnique, Montreal (Canada)

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Publications

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Li L, Ji S, Lin W. (2020) Tourmaline microboudinage: An indicator of its host rheology Journal of Structural Geology. 138: 104096
Li L, Ji S. (2020) On microboudin paleopiezometers and their applications to constrain stress variations in tectonites Journal of Structural Geology. 130: 103928
Xu Z, Li Y, Ji S, et al. (2020) Qinling gneiss domes and implications for tectonic evolution of the Early Paleozoic Orogen in Central China Journal of Asian Earth Sciences. 188: 104052
Ji S, Li L. (2019) Characterization of Stream Potholes in Interlayered Felsic and Mafic Gneisses from the Deerfield River, Shelburne Falls (Massachusetts, USA), and Implications for River Incision into Bedrock The Journal of Geology. 127: 183-205
Ji S, Wang Q, Li L. (2019) Seismic velocities, Poisson's ratios and potential auxetic behavior of volcanic rocks Tectonophysics. 766: 270-282
Ji S, Zeng W, Li L, et al. (2019) Geometrical characterization of stream potholes in sandstone from the Sunxi River (Chongqing, China) and implications for the development of bedrock channels Journal of Asian Earth Sciences. 173: 374-385
Ji S, Li L, Motra HB, et al. (2018) Poisson's Ratio and Auxetic Properties of Natural Rocks Journal of Geophysical Research. 123: 1161-1185
Yu C, Ji SY, Sha QQ, et al. (2016) BTG4 is a meiotic cell cycle-coupled maternal-zygotic-transition licensing factor in oocytes. Nature Structural & Molecular Biology
Ji S, Wang Q, Shao T, et al. (2016) S-wave velocities and anisotropy of typical rocks from Yunkai metamorphic complex and constraints on the composition of the crust beneath Southern China Tectonophysics. 686: 27-50
Shao T, Ji S, Oya S, et al. (2016) Mica-dominated seismic properties of mid-crust beneath west Yunnan (China) and geodynamic implications Tectonophysics. 677: 324-338
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