Terrane Accretion is the tectonic process whereby a distinct fragment of crustal material, originating from a different geological setting, is added to a continental margin through plate convergence and subsequent deformation, distinguishing it from in-situ crustal growth.
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Accretionary orogens through Earth history
Peter A. Cawood, Alfred Kröner, William J. Collins et al. · Geological Society London Special Publications · 2009 · 1.1K citations
Assembly of the Lhasa and Qiangtang terranes in central Tibet by divergent double subduction
Di‐Cheng Zhu, Shi-Min Li, Peter A. Cawood et al. · Lithos · 2015 · 592 citations · Full text
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Geological Survey of Canada
Ottawa, Canada
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United States Geological Survey
Reston, United States
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Chinese Academy of Geological Sciences
Beijing, China
22 h-index
60 publications
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Centre National de la Recherche Scientifique
Paris, France
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62 publications
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British Geological Survey
Nottingham, United Kingdom
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44 publications
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Curtin University
Perth, Australia
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33 publications
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Chinese Academy of Sciences
Beijing, China
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University of Arizona
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