Shear Zone Development is a structural geological process denoting the progressive localization of ductile deformation within a preferred orientation in the Earth's crust, distinguished by the systematic accumulation of strain and the formation of planar or curviplanar zones of intense shearing in thrust belt settings.
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Rheology of the lithosphere: Selected topics
S. H. Kirby, A. K. Kronenberg · Reviews of Geophysics · 1987 · 682 citations
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Centre National de la Recherche Scientifique
Paris, France
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49 publications
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ETH Zurich
Zurich, Switzerland
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University of Leeds
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22 publications
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Monash University
Melbourne, Australia
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Johannes Gutenberg University Mainz
Mainz, Germany
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Universidade Federal de Pernambuco
Recife, Brazil
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China University of Geosciences (Beijing)
Beijing, China
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Lausanne, Switzerland
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- International Journal of Earth Sciences
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