Who is Dewey, John F. (1937– ) British Tectonicist, Structural
Geologist John F. Dewey received his Ph.D. from the University
of London in 1960. He is a distinguished professor
and a member of the National Academy of Sciences. John
Dewey was one of the early scientists to pioneer the development
of the plate tectonic paradigm, offering explanations of
the Appalachian mountain belt in terms of plate tectonics and
later expanding his studies to a global scale. He presented
plate tectonic concepts in a kinematic framework, clearly
describing many phenomena for the first time. His basic
interests and knowledge are in structural geology and tectonics
from the small-scale materials science of deformed rocks
to the large-scale origin of topography and structures. Ongoing
field-based research is on the rock fabrics and structures
of transpression and transtension, especially in California,
New Zealand, Norway, Ireland, and Newfoundland. Evolving
interests are in the neotectonics of California and Nevada
in the relationship between faulting, topography, and sediment
provenance, yield, and distribution. Derivative interests are in
the geohazard of volcanoes, earthquakes, and landslides.














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