碰撞帶

碰撞帶（英語：Collision zone）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[编辑]

^ 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
^ 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

[”Gök,”-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

[Karig,”-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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