George D. Spence spends much of his time researching Clathrate hydrate, Subduction, Seismology, Continental margin and Reflection. In Subduction, he works on issues like Continental shelf, which are connected to Tectonics, Accretionary wedge and Geomorphology. His Seismology research is multidisciplinary, relying on both Buttress and Bathymetry.
His research in Continental margin intersects with topics in Seismic refraction, Rift and Igneous rock. As part of one scientific family, George D. Spence deals mainly with the area of Mineralogy, narrowing it down to issues related to the Seabed, and often Submarine pipeline. His Seafloor spreading research includes elements of Waves and shallow water, Seismic wave and Petrology.
The scientist’s investigation covers issues in Seismology, Clathrate hydrate, Seafloor spreading, Subduction and Submarine pipeline. George D. Spence combines subjects such as Seismic tomography and Crust with his study of Seismology. His Seafloor spreading study combines topics from a wide range of disciplines, such as Sedimentary rock, Ridge and Bathymetry.
His work in Subduction addresses subjects such as Continental shelf, which are connected to disciplines such as Juan de Fuca Plate. In his work, Pore water pressure is strongly intertwined with Geomorphology, which is a subfield of Submarine pipeline. The various areas that George D. Spence examines in his Mineralogy study include Seismometer, Sediment and Continental margin.
His main research concerns Seismology, Submarine pipeline, Geomorphology, Margin and Clathrate hydrate. Many of his research projects under Seismology are closely connected to Queen with Queen, tying the diverse disciplines of science together. His biological study spans a wide range of topics, including Fault, Thrust fault and Ridge.
The Submarine pipeline study combines topics in areas such as Water column, Current meter and Submarine. His Geomorphology study combines topics from a wide range of disciplines, such as Continental shelf, Juan de Fuca Plate and Outflow. George D. Spence interconnects Trough, Rift, Continental crust, Magmatism and Seismic tomography in the investigation of issues within Seafloor spreading.
His primary scientific interests are in Submarine pipeline, Seismology, Water column, Geomorphology and Outflow. His Submarine pipeline research is classified as research in Oceanography. His Subduction study in the realm of Seismology interacts with subjects such as Shear strength.
The concepts of his Water column study are interwoven with issues in Current meter and Underwater. His studies in Geomorphology integrate themes in fields like Submarine, Pore water pressure, Bathymetry and Holocene. Outflow combines with fields such as Flare, Range, Margin and Natural gas in his work.
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.
A seismic study of methane hydrate marine bottom simulating reflectors
R. D. Hyndman;G. D. Spence.
Journal of Geophysical Research (1992)
Magmatism at rifted continental margins
Robert S. White;George D. Spence;Susan R. Fowler;Dan P. McKenzie.
Nature (1987)
Velocity structure of a gas hydrate reflector.
Satish C. Singh;Timothy A. Minshull;George D. Spence.
Science (1993)
Decreased stability of methane hydrates in marine sediments owing to phase-boundary roughness.
W. T. Wood;J. F. Gettrust;N. R. Chapman;G. D. Spence.
Nature (2002)
Tectonic sediment thickening, fluid expulsion, and the thermal regime of subduction zone accretionary prisms: The Cascadia Margin off Vancouver Island
R. D. Hyndman;K. Wang;T. Yuan;G. D. Spence.
Journal of Geophysical Research (1993)
The Hatton Bank continental margin—II. Deep structure from two-ship expanding spread seismic profiles
S. R. Fowler;R. S. White;G. D. Spence;G. K. Westbrook.
Geophysical Journal International (1989)
Seismic structure across the active subduction zone of western Canada
G. D. Spence;R. M. Clowes;R. M. Ellis.
Journal of Geophysical Research (1985)
Seismic velocity studies of a gas hydrate bottom-simulating reflector on the northern Cascadia continental margin: Amplitude modeling and full waveform inversion
T. Yuan;G. D. Spence;R. D. Hyndman;T. A. Minshull.
Journal of Geophysical Research (1999)
Geophysical and geochemical signatures associated with gas hydrate–related venting in the northern Cascadia margin
Michael Riedel;Ivana Novosel;George D. Spence;Roy D. Hyndman.
Geological Society of America Bulletin (2006)
Are rupture zone limits of great subduction earthquakes controlled by upper plate structures? Evidence from multichannel seismic reflection data acquired across the northern Ecuador–southwest Colombia margin
Jean-Yves Collot;Boris Marcaillou;Françoise Sage;François Michaud.
Journal of Geophysical Research (2004)
If you think any of the details on this page are incorrect, let us know.
We appreciate your kind effort to assist us to improve this page, it would be helpful providing us with as much detail as possible in the text box below:
University of Victoria
GEOMAR Helmholtz Centre for Ocean Research Kiel
University of British Columbia
Geological Survey of Canada
Geological Survey of Canada
United States Geological Survey
Chinese Academy of Sciences
Japan Agency for Marine-Earth Science and Technology
Geological Survey of Canada
Dalhousie University
Federal Reserve Bank of New York
University of L'Aquila
Rensselaer Polytechnic Institute
Technical University of Munich
University of Oregon
University of Sheffield
University of Regensburg
University of Giessen
National Institutes of Health
Sukachev Institute of Forest
Georgia Institute of Technology
Université Paris Cité
Montreal Heart Institute
University of California, Los Angeles
University of California, San Francisco
German Institute for Economic Research