His primary areas of investigation include Seismology, Crust, Lithosphere, Subduction and Suture. His biological study spans a wide range of topics, including Basement, Tectonics and Collision zone. When carried out as part of a general Lithosphere research project, his work on Delamination is frequently linked to work in Plateau, therefore connecting diverse disciplines of study.
James Mechie frequently studies issues relating to Mantle and Subduction. His Mantle study is concerned with the larger field of Geophysics. His Suture study often links to related topics such as Terrane.
The scientist’s investigation covers issues in Seismology, Crust, Lithosphere, Subduction and Mantle. His Seismology study frequently draws connections between related disciplines such as Structural basin. His Crust research is multidisciplinary, relying on both Transform fault, Suture, Petrology, Underplating and Terrane.
In general Lithosphere, his work in Asthenosphere is often linked to Hindu kush linking many areas of study. His study in Subduction is interdisciplinary in nature, drawing from both Slab and Induced seismicity, Seismic zone. His Mantle research focuses on subjects like Transition zone, which are linked to Continental margin.
Seismology, Crust, Lithosphere, Subduction and Terrane are his primary areas of study. His work on Slab expands to the thematically related Seismology. His Crust study incorporates themes from Ophiolite and Receiver function.
His research ties Mantle and Lithosphere together. James Mechie has researched Mantle in several fields, including Discontinuity and Petrology. His Subduction study which covers Continental crust that intersects with Geophysical imaging and Xenolith.
His primary areas of study are Seismology, Crust, Lithosphere, Subduction and Mantle. His Seismology research includes themes of Attenuation tomography and Seismic tomography. Geophysics covers he research in Crust.
His Lithosphere research is multidisciplinary, incorporating elements of Slab and Continental margin. His work carried out in the field of Subduction brings together such families of science as Seamount and Terrane. His research integrates issues of Lehmann discontinuity, Discontinuity, Laurentia and Craton in his study of Mantle.
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Partially Molten Middle Crust Beneath Southern Tibet: Synthesis of Project INDEPTH Results
K. D. Nelson;Wenjin Zhao;L. D. Brown;J. Kuo.
Science (1996)
Seismic Images of Crust and Upper Mantle Beneath Tibet: Evidence for Eurasian Plate Subduction
R. Kind;X. Yuan;J. Saul;D. Nelson.
Science (2002)
Lithospheric and upper mantle structure of southern Tibet from a seismological passive source experiment
Xiaohui Yuan;James Ni;Rainer Kind;James Mechie.
Journal of Geophysical Research (1997)
Crustal structure of central Tibet as derived from project INDEPTH wide-angle seismic data
W. Zhao;J. Mechie;L. D. Brown;J. Guo.
Geophysical Journal International (2001)
Seismic polarization anisotropy beneath the central Tibetan Plateau
Wei-Chuang Huang;James F. Ni;Frederik Tilmann;Doug Nelson.
Journal of Geophysical Research (2000)
Tibetan plate overriding the Asian plate in central and northern Tibet
Wenjin Zhao;Prakash Kumar;James Mechie;Rainer Kind.
Nature Geoscience (2011)
INDEPTH III seismic data: From surface observations to deep crustal processes in Tibet
Seth S. Haines;Simon L. Klemperer;Larry Brown;Guo Jingru.
Tectonics (2003)
Geometry of the Pamir-Hindu Kush intermediate-depth earthquake zone from local seismic data
Christian Sippl;B Schurr;X. Yuan;J. Mechie.
Journal of Geophysical Research (2013)
Seismic imaging of subducting continental lower crust beneath the Pamir
F. Schneider;X. Yuan;B Schurr;J. Mechie.
Earth and Planetary Science Letters (2013)
Injection of Tibetan crust beneath the south Qaidam Basin: Evidence from INDEPTH IV wide-angle seismic data
M. S. Karplus;W. Zhao;S. L. Klemperer;Z. Wu.
Journal of Geophysical Research (2011)
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