Sidao Ni focuses on Seismology, Mantle, Shear, Geophysics and Aftershock. His work in Seismology is not limited to one particular discipline; it also encompasses Rayleigh wave. His Mantle study incorporates themes from East African Rift and Indian ocean.
His Shear research is multidisciplinary, incorporating elements of Mineralogy, Broadband and Latitude, Geodesy. His work on Synthetic seismogram as part of general Geophysics study is frequently linked to Earth, bridging the gap between disciplines. His work in Aftershock addresses issues such as Slip, which are connected to fields such as Trough, Plate tectonics, Seismogram and Submarine pipeline.
Sidao Ni mostly deals with Seismology, Mantle, Geodesy, Aftershock and Rayleigh wave. His Seismology research integrates issues from Amplitude and Surface wave. His studies in Mantle integrate themes in fields like Crust, Plume, Upwelling and Anisotropy.
His Aftershock research is multidisciplinary, relying on both Slip, Hypocenter, Fault and Inversion. His research in Slip is mostly concerned with Seismic moment. The study incorporates disciplines such as Seismic wave and Coda in addition to Seismogram.
His primary scientific interests are in Seismology, Ambient noise level, Mantle, Geophysics and Sequence. Sidao Ni undertakes multidisciplinary studies into Seismology and Directivity in his work. Sidao Ni has included themes like Attenuation and Seismic wave in his Mantle study.
Sidao Ni interconnects Seismic tomography, Large Low Shear Velocity Provinces, Stishovite and Scale in the investigation of issues within Seismic wave. His study in Geophysics is interdisciplinary in nature, drawing from both Surface finish, Circulation and Oceanic crust. As a member of one scientific family, Sidao Ni mostly works in the field of Inversion, focusing on Rayleigh wave and, on occasion, Seismic array.
His main research concerns Seismology, Seismic wave, Geophysics, Mantle and Mineralogy. Induced seismicity and Aftershock are the primary areas of interest in his Seismology study. The various areas that he examines in his Seismic wave study include Surface finish, Mantle convection, Amplitude, Tangential and normal components and Attenuation.
His studies deal with areas such as Circulation and Scale as well as Geophysics. His Mantle research is multidisciplinary, incorporating perspectives in Subduction, Oceanic crust, Large Low Shear Velocity Provinces and Stishovite. In his works, Sidao Ni undertakes multidisciplinary study on Mineralogy and Phase.
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Rupture Process of the 2004 Sumatra-Andaman Earthquake
Charles J. Ammon;Chen Ji;Hong-Kie Thio;David Robinson.
Science (2005)
Sharp sides to the African superplume.
Sidao Ni;Eh Tan;Michael Gurnis;Don Helmberger.
Science (2002)
Source mechanism of strong aftershocks (Ms≥5.6) of the 2008/05/12 Wenchuan earthquake and the implication for seismotectonics
Yong Zheng;Hong Sheng Ma;Jian Lü;Si Dao Ni.
Science in China Series D: Earth Sciences (2009)
Seismology: Energy radiation from the Sumatra earthquake
Sidao Ni;Sidao Ni;Hiroo Kanamori;Don Helmberger.
Nature (2005)
Evidence for strong shear velocity reductions and velocity gradients in the lower mantle beneath Africa
Jeroen Ritsema;Sidao Ni;Donald V. Helmberger;H. Philip Crotwell.
Geophysical Research Letters (1998)
Retrieval of Moho‐reflected shear wave arrivals from ambient seismic noise
Zhongwen Zhan;Zhongwen Zhan;Sidao Ni;Don V. Helmberger;Robert W. Clayton.
Geophysical Journal International (2010)
Seismological constraints on the South African superplume; could be the oldest distinct structure on earth
Sidao Ni;Don V. Helmberger.
Earth and Planetary Science Letters (2003)
The Pawnee earthquake as a result of the interplay among injection, faults and foreshocks.
Xiaowei Chen;Nori Nakata;Colin Pennington;Jackson Haffener.
Scientific Reports (2017)
Three-dimensional structure of the African superplume from waveform modelling
Sidao Ni;Sidao Ni;Don V. Helmberger;Jeroen Tromp.
Geophysical Journal International (2005)
Ridge‐like lower mantle structure beneath South Africa
Sidao Ni;Don V. Helmberger.
Journal of Geophysical Research (2003)
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