Collisional Orogeny is a tectonic process, within the broader class of orogenic mechanisms, distinguished by the crustal thickening and mountain formation resulting from the convergent collision of two continental plates, typically following the closure of an ocean basin.
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Xinmin Zhou, Tao Sun, Weizhou Shen et al. · Episodes · 2006 · 1.7K citations · Full text
Tethyan sutures of northern Turkey
Aral İ. Okay, Okan Tüysüz · Geological Society London Special Publications · 1999 · 1.1K citations
Zagros orogeny: a subduction-dominated process
Philippe Agard, Jafar Omrani, Laurent Jolivet et al. · Geological Magazine · 2011 · 960 citations · Full text
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