碰撞帶

碰撞帶（英語：） 是指當構造板塊都帶有大陸岩石圈，在聚合板塊邊緣相遇時，就會出現碰撞帶。大陸岩石圈由於密度相對較低而通常不會向下俯衝，因此大陸地殼塊會堆積在俯衝帶上方，導致一個複雜的造山運動區域，涉及褶皺和逆衝斷層。列如東安納托利亞碰撞帶[1]和班達弧-澳大利亞碰撞帶[2]。

參考文獻
  1. 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
  2. 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; pp. 18–32
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