His primary scientific interests are in Shear zone, Crust, Geochemistry, Coesite and Mineralogy. His work on Petrology expands to the thematically related Shear zone. His Crust research includes elements of Seismic anisotropy and Terrane.
His research investigates the connection with Geochemistry and areas like Eclogite which intersect with concerns in Continental crust. In his study, Metamorphism is inextricably linked to Dislocation creep, which falls within the broad field of Coesite. The concepts of his Mineralogy study are interwoven with issues in Slip and Dynamic recrystallization.
Shaocheng Ji mostly deals with Mineralogy, Geochemistry, Crust, Petrology and Metamorphic rock. His biological study spans a wide range of topics, including Lineation, Mylonite and Quartz, Plagioclase. His research in Geochemistry intersects with topics in Eclogite and Terrane.
His Crust research includes themes of Seismology, Rift, Shear zone and Seismic anisotropy. Shaocheng Ji has included themes like Shear and Craton in his Shear zone study. His Metamorphic rock research incorporates elements of Felsic, Mantle and Lithology.
Shaocheng Ji spends much of his time researching Geochemistry, Petrology, Seismic anisotropy, Crust and Metamorphic rock. The study incorporates disciplines such as Ophiolite, Eclogite and Terrane in addition to Geochemistry. The various areas that Shaocheng Ji examines in his Petrology study include Volcano, Rhyolite and Volcanic rock.
Shaocheng Ji interconnects Seismology, Shear wave splitting, Mineralogy and Gabbro in the investigation of issues within Seismic anisotropy. His Crust study combines topics in areas such as Lineation, Mylonite, Yield and Underplating. Shaocheng Ji combines subjects such as Metamorphism and Zircon with his study of Metamorphic rock.
Shaocheng Ji spends much of his time researching Seismic anisotropy, Geochemistry, Mineralogy, Shear wave splitting and Seismology. His studies deal with areas such as Ophiolite and Eclogite as well as Geochemistry. His Mineralogy study integrates concerns from other disciplines, such as Grain boundary, Porosity and Amphibole.
To a larger extent, he studies Petrology with the aim of understanding Shear wave splitting. Shaocheng Ji is studying Metamorphic rock, which is a component of Petrology. His studies in Simple shear integrate themes in fields like Tectonics, Shear zone, Transpression and Lithosphere.
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The Ailao Shan-Red River shear zone (Yunnan, China), Tertiary transform boundary of Indochina
Philippe Hervé Leloup;Robin Lacassin;Paul Tapponnier;Urs Schärer.
Tectonophysics (1995)
Zircon U-Pb geochronology of gneissic rocks in the Yunkai massif and its implications on the Caledonian event in the South China Block
Yuejun Wang;Yuejun Wang;Weiming Fan;Guochun Zhao;Shaocheng Ji.
Gondwana Research (2007)
Uplift of the Longmen Shan Range and the Wenchuan Earthquake
Zhiqin Xu;Shaocheng Ji;Haibing Li;Liwei Hou.
Episodes (2008)
Handbook of seismic properties of minerals, rocks and ores
Shaocheng Ji;Qin Wang;Bin Xia.
(2002)
A revised model for the relationship between joint spacing and layer thickness
Shaocheng Ji;Kazuko Saruwatari.
Journal of Structural Geology (1998)
Composition and tectonic evolution of the Chinese continental crust constrained by Poisson's ratio
Shaocheng Ji;Qian Wang;Matthew H. Salisbury.
Tectonophysics (2009)
Indosinian high-strain deformation for the Yunkaidashan tectonic belt, south China : Kinematics and 40Ar/39Ar geochronological constraints
Yuejun Wang;Yuejun Wang;Weiming Fan;Peter Anthony Cawood;Shaocheng Ji.
Tectonics (2007)
Ductility of garnet as an indicator of extremely high temperature deformation
Shaocheng Ji;Jacques Martignole.
Journal of Structural Geology (1996)
Archaean cratonic roots, mantle shear zones and deep electrical anisotropy
M. Mareschal;R. L. Kellett;R. L. Kellett;R. D. Kurtz;J. N. Ludden;J. N. Ludden.
Nature (1995)
Kinematics and dynamics of the Namche Barwa Syntaxis, eastern Himalaya: Constraints from deformation, fabrics and geochronology
Zhiqin Xu;Shaocheng Ji;Zhihui Cai;Lingsen Zeng.
Gondwana Research (2012)
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