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John Suppe (born 1942) is an American geologist who is Distinguished Professor of Geology at University of Houston and Princeton University.
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John Suppe (born 1942) is an American geologist who is Distinguished Professor of Geology at University of Houston and Princeton University.
He received his B.A. from University of California, Riverside in 1965, and his Ph.D. from Yale University in 1969. He joined the Princeton faculty in 1971, and was the chairman of the Department of Geology from 1991 to 1993. He transferred to emeritus status, and moved to Taiwan where he became a Distinguished Chair Research Professor at the National Taiwan University in 2007. [1]
Suppe's research specialties are structural geology and tectonics, and he is best known for his work on "fault-related folding" theories with his two classical papers "Geometry and kinematics of fault-bend folding" and "Geometry and kinematics of fault-propagation folding". [2] Additionally, Suppe is also well known for his extensive work on the formation of mountain belts with examples from California, Taiwan, and China.
Suppe has been former visiting professor at the National Taiwan University, the California Institute of Technology, Barcelona University, and Munich University. Furthermore he was a NASA Guest Investigator for the analysis of the Venus images from the Magellan mission.
John Suppe is also a Christian who has written on the relationship between science and religion in articles like Thoughts on the Epistemology of Christianity in Light of Science. [3]
Among his awards and honors, he received the Best Publication Award in Structural Geology and Tectonics from the Geological Society of America in 1986 and 1996, the Alexander von Humboldt Foundation research prize in 2006, the Wilbur Lucius Cross Medal from the Yale Graduate School in 2007 and the Career Contribution Award in Structural Geology and Tectonics from the Geological Society of America in 2008. Suppe has been a member of the United States National Academy of Sciences since 1995. In 2019, Suppe was named a Fellow of the American Geophysical Union. [4]
Kenneth Jinghwa Hsu Ph.D, M.A., born 28 June 1929, is a Chinese scientist, geologist, paleoclimatologist, oceanographer, government advisor, author, inventor and entrepreneur who was born in Nanjing, China.
Eldridge Moores was an American geologist. He specialized in the understanding of ophiolites and the geology of the continental crust of the Western United States and Tethyan belt, the geology of Greece, Cyprus, and Pakistan, and the tectonic development of the Sierra Nevada and the Alpine - Himalayan systems.
Tanya Atwater is an American geophysicist and marine geologist who specializes in plate tectonics. She is particularly renowned for her early research on the plate tectonic history of western North America.
Burrell Clark Burchfiel is an American structural geologist. Born in Stockton, California, he earned his Ph.D. in 1961 at Yale University. His first academic appointment was to the Geology department at Rice University. He is the Schlumberger Professor Emeritus of Geology at MIT. Research interests: Origin, development, and structural evolution of the continental crust. His current work involves study of the geological history and evolution of the Tibetan plateau.
Raymond Alexander Price, is a Canadian geologist. He has used his research on the structure and tectonics of North America’s lithosphere to produce extensive geological maps. He has also provided guidance for nuclear fuel waste disposal and reports on the human contribution to Global warming.
James Anthony Jackson CBE FRS is Professor of Active Tectonics and head of Bullard Laboratories, Department of Earth Sciences, Cambridge University. He made his name in geophysics, using earthquake source seismology to examine how continents are deformed. His central research focus is to observe the active processes shaping our continents.
Mary Lou Zoback is an American geophysicist who led the world stress map project of the International Lithosphere Program. Zoback is currently a member of the U.S. Nuclear Waste Technical Review Board.
Kerry E. Sieh is an American geologist and seismologist.
A detachment fold, in geology, occurs as layer parallel thrusting along a decollement develops without upward propagation of a fault; the accommodation of the strain produced by continued displacement along the underlying thrust results in the folding of the overlying rock units. As a visual aid, picture a rug on the floor. By placing your left foot on one end and pushing towards the other end of the rug, the rug slides across the floor (decollement) and folds upward. Figure 1, is a generalized representation of the geometry assumed by a detachment fault.
Sharon Mosher is an American geologist. She did her undergraduate work at University of Illinois Urbana-Champaign. After earning an MSc from Brown University, she returned to the University of Illinois to get her PhD in Geology in 1978. Since 2001 she has held the William Stamps Farish Chair at University of Texas, and, since 2009 she has served as the dean of the Jackson School of Geosciences at Texas. In 2013 she became the president of the American Geosciences Institute.
The Main Central Thrust is a major geological fault where the Indian Plate has pushed under the Eurasian Plate along the Himalaya. The fault slopes down to the north and is exposed on the surface in a NW-SE direction (strike). It is a thrust fault that continues along 2900 km of the Himalaya mountain belt.
David D. Pollard is a professor in geomechanics and structural geology at Stanford University.
In geology, 3D fold evolution is the study of the full three dimensional structure of a fold as it changes in time. A fold is a common three-dimensional geological structure that is associated with strain deformation under stress. Fold evolution in three dimensions can be broadly divided into two stages, namely fold growth and fold linkage. The evolution depends on fold kinematics, causes of folding, as well as alignment and interaction of the each structure with respect to each other. There are several ways to reconstruct the evolution progress of folds, notably by using depositional evidence, geomorphological evidence and balanced restoration. Understanding the evolution of folds is important because it helps petroleum geologists to gain a better understanding on the distribution of structural traps of hydrocarbon.
Kshitindramohan Naha (1932–1996) was an Indian geologist and a professor and CSIR Emeritus scientist at the Indian Institute of Technology, Kharagpur. He was known for his studies on structural geology of Precambrian era and was an elected fellow of the Indian National Science Academy, and the Indian Academy of Sciences. The Council of Scientific and Industrial Research, the apex agency of the Government of India for scientific research, awarded him the Shanti Swarup Bhatnagar Prize for Science and Technology, one of the highest Indian science awards for his contributions to Earth, Atmosphere, Ocean and Planetary Sciences in 1972.
Subir Kumar Ghosh (1932–2008) was an Indian structural geologist and an emeritus professor at Jadavpur University. He was known for his studies on theoretical and experimental structural geology and was an elected fellow of the Indian National Science Academy, and the Indian Academy of Sciences. The Council of Scientific and Industrial Research, the apex agency of the Government of India for scientific research, awarded him the Shanti Swarup Bhatnagar Prize for Science and Technology, one of the highest Indian science awards for his contributions to Earth, Atmosphere, Ocean and Planetary Sciences in 1977.
Richard Hugh Sibson is a New Zealand structural geologist and emeritus professor at the University of Otago, who has received numerous honors and awards for his work in the field of earthquake research. He has caused a 'fundamental shift' in the interpretation of the relationship between earthquakes and fault zone geology and on the origin of fault-hosted mineral deposits.
Whitney Maria Behr is an American Earth Scientist known for her contributions to understanding mechanics and kinematics of deformation in Earth's lithosphere. She was educated in the United States following which she held academic positions there. Since 2018, she has been the chair of the Structural Geology & Tectonics Group in the Geological Institute at ETH Zürich.
Delores Marie Robinson is an American geophysicist who is a professor and department chair at the University of Alabama. Her research considers how orogenic systems evolve from porto-magmatic arcs, with a particular focus on Western Nepal, India, Bhutan and Southern Tibet.
An Yin is a Chinese-American Earth scientist and a Professor of Geology at the University of California, Los Angeles (UCLA). His early work explores the mechanical origin and kinematic evolution of low-angle normal faults and thrust systems in the North American Cordillera. He is perhaps best known for his work on the tectonic evolution of the Himalayas and Tibetan plateau. His research interests have shifted in recent years to slow-earthquake mechanics, early Earth tectonics, and planetary studies.
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