Roger Clive Searle
Professor
Department of Earth Sciences
Durham University
United Kingdom
Biography
1966: BA, University of Cambridge (Natural Sciences Tripos, Part II Physics); MA, 1970 1969: Ph.D., University of Newcastle-upon-Tyne (Geophysics) 1970: Assistant Professor, Haile Sellassie I University, Addis Ababa, Ethiopia 1973: Senior Scientific Officer, Institute of Oceanographic Sciences 1978: Principal Scientific Officer, Institute of Oceanographic Sciences 1989: Senior Principal Scientific Officer (Grade 6 Individual Merit), Institute of Oceanographic Sciences 1989-2011: Professor of Geophysics, University of Durham 2011-present: Professor of Geophysics (Emeritus), University of Durham
Research Interest
Roger Searle has an international reputation in the use of imaging sonars and other geophysical methods to understand tectonic and magmatic processes on the ocean floor, particularly at mid-ocean ridge spreading centres. His early work included the definition of plate boundaries to sub-kilometre resolution and determining the evolution of propagating rifts and oceanic microplates.He has studied the effects of mantle hot spots on plate accretion processes. Recently he has worked on the detailed tectonic patterns and volcanic systems of spreading centres, especially at Oceanic Core Complexes and ultra-slow spreading rates. Roger has published over 120 peer-reviewed articles and is a regular contributor to international conferences.
Publications
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C Mallows & R C Searle (2012). A geophysical study of oceanic core complexes and surrounding terrain, Mid-Atlantic Ridge 13°-14°N. Geochemistry, Geophysics, Geosystems
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Yeo, I. A. & Searle, R. C. (2013). High-resolution Remotely Operated Vehicle (ROV) mapping of a slow-spreading ridge: Mid-Atlantic Ridge 45°N. Geochemistry geophysics geosystems 14(6): 1693-1702.
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Sauter, D, Cannat, M, Rouméjon, S, Andreani, M, Birot, D, Bronner, A, Brunelli, D, Carlut, J, Delacour, A, Guyader, V, MacLeod, C, Manatschal, G, Mendel, V, Ménez, B, Pasini, V, Ruellan, E & Searle, R (2013). Continuous exhumation of mantle-derived rocks at the Southwest Indian Ridge for 11 million years. Nature Geoscience 6(4): 314-320.