碰撞带

碰撞带（英语：Collision zone）是指当构造板块都带有大陆岩石圈，在聚合板块边缘相遇时，就会出现碰撞带。大陆岩石圈由于密度相对较低而通常不会向下俯冲，因此大陆地壳块会堆积在俯冲带上方，导致一个复杂的造山运动区域，涉及褶皱和逆冲断层。列如东安纳托利亚碰撞带^[1]和班达弧-澳大利亚碰撞带^[2]。

参考文献

^ 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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