彎曲造山帶
參考文獻

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↑  Troy Smith, Gideon Rosenbaum, Lutz Gross （2021）
Formation of oroclines by buckling continental ribbons: Fact or fiction?,Tectonophysics,Volume 814,2021,228950,ISSN 0040-1951,https://doi.org/10.1016/j.tecto.2021.228950.
(https://www.sciencedirect.com/science/article/pii/S0040195121002328)
↑  Robert J. (2015） Musgrave,Oroclines in the Tasmanides,Journal of Structural Geology,Volume 80, Pages 72-98,ISSN 0191-141,https://doi.org/10.1016/j.jsg.2015.08.010.
(https://www.sciencedirect.com/science/article/pii/S0191814115300286)
↑  M. Rezaeian, C.B. Kuijper, A. van der Boon, D. Pastor-Galán, L.J. Cotton, C.G. Langereis, W. Krijgsman （2020）
Post-Eocene coupled oroclines in the Talesh (NW Iran): Paleomagnetic constraints,Tectonophysics,Volume 786,2020,ISSN 0040-1951,https://doi.org/10.1016/j.tecto.2020.228459.
(https://www.sciencedirect.com/science/article/pii/S0040195120301426)
↑  Isacks, Bryan L. (1988), "Uplift of the Central Andean Plateau and Bending of the Bolivian Orocline" (PDF), Journal of Geophysical Research, 93 (B4): 3211–3231, doi:10.1029/jb093ib04p03211
↑  Kley, J. (1999), "Geologic and geometric constraints on a kinematic model of the Bolivian orocline", Journal of South American Earth Sciences, 12 (2): 221–235, doi:10.1016/s0895-9811(99)00015-2
↑  Beck, Myrl E. (1987), "Tectonic rotations on the leading edge of South America: The Bolivian orocline revisited", Geology, 15 (9): 806–808, doi:10.1130/0091-7613(1987)15<806:trotle>2.0.co;2
↑  Prezzi, Claudia B.; Vilas, Juan F. (1998). "New evidence of clockwise vertical axis rotations south of the Arica elbow (Argentine Puna)". Tectonophysics. 292 (1–2): 85–100. doi:10.1016/s0040-1951(98)00058-4.
↑  Arriagada, César; Ferrando, Rodolfo; Córdova, Loreto; Morata, Diego; Roperch, Pierrick (2013), "The Maipo Orocline: A first scale structural feature in the Miocene to Recent geodynamic evolution in the central Chilean Andes" (PDF), Andean Geology, 40 (3): 419–437
↑  Jara-Muñoz, Julius; Melnick, Daniel; Dominik, Brill; Strecker, Manfred R. (2015), "Segmentation of the 2010 Maule earthquake rupture from a joint analysis of uplifted marine terraces and seismic cycle deformation", Quaternary Science Reviews, 113: 171–192, doi:10.1016/j.quascirev.2015.01.005的一個微妙的山脊。它標誌著安第斯山脈的一個向海凸出的彎道
↑  Lahtinen, R.; Sayab, M.; Johnston, S.T. (2016). "Inari orocline – progressive or secondary orocline". Institute of Seismology, University of Helsinki Report S-65. Lithosphere 2016 Ninth Symposium on the structure, composition and evolution of the lithosphere in Fennosscandia. pp. 69–74.
↑  Lahtinen, R.; Sayab, M.; Johnston, S.T. (2016). "Inari orocline – progressive or secondary orocline". Institute of Seismology, University of Helsinki Report S-65. Lithosphere 2016 Ninth Symposium on the structure, composition and evolution of the lithosphere in Fennosscandia. pp. 69–74.
↑  Gutiérrez-Alonso, G.; Johnston, S.T.; Weil, A.B.; Pastor-Galán, D.; Fernández-Suárez, J. (2012)
↑   "Buckling an orogen: The Cantabrian Orocline" (PDF). GSA Today. 22 (7): 4–9. oi:10.1130/GSATG141A.1
↑  Cayley, R. (2014). "The Lachlan Orocline of Eastern Australia. Giant folds, the geodynamic processes that can form them, and how these new understandings have potential to revolutionise the resource prospectivity game in Eastern Australia". New Perspectives Workshop, September 2014. Australian Institute of Geoscientists. Retrieved 4 March 2018
↑  Chengxin Jiang; Yingjie Yang; Yong Zheng (2016). "Crustal structure in the junction of Qinling Orogen, Yangtze Craton and Tibetan Plateau: implications for the formation of the Dabashan Orocline and the growth of Tibetan Plateau". Geophysical Journal International. 205 (3): 1670–1681. doi:10.1093/gji/ggw096