The scientist’s investigation covers issues in Seismology, Subduction, Fault, Focal mechanism and Tectonics. His work on Seismology is being expanded to include thematically relevant topics such as Permeability. His work on Episodic tremor and slip as part of general Subduction research is frequently linked to Return period, bridging the gap between disciplines.
His Fault study combines topics in areas such as Petrology and Pressure gradient. His Focal mechanism research includes elements of Fault mechanics, Stress field, Seismic anisotropy and Geodesy. His Lithosphere, Inversion and Mountain formation study in the realm of Tectonics connects with subjects such as Strain rate.
John Townend mainly investigates Seismology, Fault, Induced seismicity, Subduction and Petrology. The Seismology study combines topics in areas such as Shear and Crust. John Townend has included themes like Intraplate earthquake and Lithosphere in his Crust study.
The Strike-slip tectonics research he does as part of his general Fault study is frequently linked to other disciplines of science, such as Drill site, therefore creating a link between diverse domains of science. His study looks at the relationship between Subduction and fields such as Focal mechanism, as well as how they intersect with chemical problems. John Townend combines subjects such as Geothermal gradient, Outcrop, Cataclasite and Permeability with his study of Petrology.
His main research concerns Seismology, Fault, Induced seismicity, Earthquake catalog and Peninsula. His Seismology study combines topics in areas such as Shear and Geothermal gradient. John Townend has researched Shear in several fields, including Seismic noise and Seismic moment.
The study incorporates disciplines such as Thermal, Geomorphology and Earthquake detection in addition to Fault. His research integrates issues of Mylonite, Schist and Petrology, Lithology in his study of Thermal. His Induced seismicity research is multidisciplinary, relying on both Quartz and Crust.
His scientific interests lie mostly in Shear, Seismology, Real-time computing, Statistical model and Aquifer. His Shear study incorporates themes from Seismic noise, Geothermal gradient, Volcano and Convergent boundary. His study in Seismology focuses on Seismic moment in particular.
His Statistical model research overlaps with Groundwater and Soil science.
This overview was generated by a machine learning system which analysed the scientist’s body of work. If you have any feedback, you can contact us here.
How faulting keeps the crust strong
John Townend;Mark D. Zoback.
Geology (2000)
Implications of hydrostatic pore pressures and high crustal strength for the deformation of intraplate lithosphere
Mark D. Zoback;John Townend.
Tectonophysics (2001)
Ambient noise Rayleigh wave tomography of New Zealand
Fan Chi Lin;Michael H. Ritzwoller;John Townend;Stephen Bannister.
Geophysical Journal International (2007)
Regional tectonic stress near the San Andreas fault in central and southern California
J. Townend;M. D. Zoback.
Geophysical Research Letters (2004)
Calculating horizontal stress orientations with full or partial knowledge of the tectonic stress tensor
Björn Lund;John Townend.
Geophysical Journal International (2007)
Do great earthquakes occur on the Alpine fault in central South Island, New Zealand?
R. Sutherland;D. Eberhart‐Phillips;R. A. Harris;T. Stern.
Geophysical monograph (2013)
Characterizing the seismogenic zone of a major plate boundary subduction thrust: Hikurangi Margin, New Zealand
Laura M. Wallace;Martin Reyners;Ursula Cochran;Stephen Bannister.
Geochemistry Geophysics Geosystems (2009)
Slow slip on the northern Hikurangi subduction interface, New Zealand
Annie Douglas;J. Beavan;L. Wallace;J. Townend.
Geophysical Research Letters (2005)
Stress, strain, and mountain building in central Japan
John Townend;Mark D. Zoback.
Journal of Geophysical Research (2006)
Steady-State Failure Equilibrium and Deformation of Intraplate Lithosphere
Mark D. Zoback;John Townend;Balz Grollimund.
International Geology Review (2002)
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