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Collision zone : ウィキペディア英語版 | Collision zone A collision zone occurs when tectonic plates meeting at a convergent boundary both bearing continental lithosphere. As continental lithosphere is usually not subducted due to its relative low density, the result is a complex area of orogeny involving folding and thrust faulting as the blocks of continental crust ''pile up'' above the subduction zone. ==Examples==
Notable examples include: * Philippine Mobile Belt * Molucca Sea Collision Zone * Izu Collision Zone * Ishikari Collision Zone * Mount Fuji Collision Zone * Carlin Unconformity * Daisetsuzan Collision Zone * Luzon-Taiwan Collision Zone * Indus-Yarlung suture zone * Eastern Anatolian collision zone〔 R Gök, R., et al. ''Lithospheric structure of the continent–continent collision zone: eastern Turkey,'' Geophysical Journal International, 2007, Volume 169, Issue 3, Pages 789–1378〕 * Banda Arc–Australian collision zone〔Karig, Daniel E., et al., ''Nature and distribution of deformation across the Banda Arc–Australian collision zone at Timor,'' GSA Bulletin; January 1987; v. 98; no. 1; p. 18-32〕
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