Wen, Lianxing - Department of Geosciences, SUNY at Stony Brook

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Wen, Lianxing - Department of Geosciences, SUNY at Stony Brook

Geographic boundary and shear wave velocity structure of the "Pacific anomaly" near the coremantle boundary
Upper mantle SH-and P-velocity structures and compositional models beneath southern Africa
Geometry and P and S velocity structure of the ``African and Lianxing Wen1
Mapping the geometry and geographic distribution of a very low velocity province at the base of the Earth's mantle
Seismic velocity and attenuation structures in the top 400 km of the Earth's inner core along equatorial paths
An SH hybrid method and shear velocity structures in the lowermost mantle beneath the central Pacific
Inner core attenuation anisotropy Wen-che Yu , Lianxing Wen
Complex seismic anisotropy at the border of a very low velocity province at the base of the Earth's mantle
Structural features and shear-velocity structure of the ``Pacific Anomaly''
A two-dimensional hybrid method for modeling seismic wave propagation in anisotropic media
Geophys. J. Int. (2007) 169, 866896 doi: 10.1111/j.1365-246X.2007.03274.x GJIGeodesy,potentialfieldandappliedgeophysics
A compositional anomaly at the Earth's coremantle boundary as an anchor to the relatively slowly moving surface hotspots
A wave equation migration method for receiver function imaging: Seismological Laboratory, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
Seismic evidence for a rapidly varying compositional anomaly at the base of the Earth's mantle beneath the Indian Ocean
Seismic evidence for a thermo-chemical boundary at the base of the Earth's mantle
Nature Macmillan Publishers Ltd 1998 letters to nature
Ultra-Low Velocity Zones Near the Core-Mantle Boundary from Broadband PKP Precursors
Z .Earth and Planetary Science Letters 146 1997 367377 Layered mantle convection: A model for geoid and topography
SH velocity and compositional models near the 660-km discontinuity beneath South America and northeast Asia
Complex seismic anisotropy in the top of the Earth's inner core beneath Africa
26 Seismological Research Letters Volume 81, Number 1 January/February 2010 doi: 10.1785/gssrl.81.1.26 INTRODUCTION
A wave equation migration method for receiver function imaging: 2. Application to the Japan subduction zone
Seismic velocity structures and detailed features of the D00 discontinuity