造山運動
注釋

↑  Tony Waltham.  3rd. Taylor & Francis. 2009: 20  [2010-05-07]. ISBN 0415469597. （原始内容存档于2021-05-09）.
1 2  Philip Kearey, Keith A. Klepeis, Frederick J. Vine. .  3rd. Wiley-Blackwell. 2009: 287  [2010-05-07]. ISBN 1405107774. （原始内容存档于2021-05-09）.
↑  
N. H. Woodcock, Robin A. Strachan. . . Wiley-Blackwell. 2000: 202, Figure 12.11. ISBN 0632036567.
↑  Frank Press.  4th. Macmillan. 2003: 468–469  [2010-05-07]. ISBN 0716796171. （原始内容存档于2021-01-29）.
↑  Gerald Schubert, Donald Lawson Turcotte, Peter Olson. . . Cambridge University Press. 2001: 35–36  [2010-05-07]. ISBN 0521798361. （原始内容存档于2021-04-13）.
↑  PA Allen. . . Wiley-Blackwell. 1997: 36 ff  [2010-05-07]. ISBN 0632035072. （原始内容存档于2021-03-20）.
↑  Gerard V. Middleton, Peter R. Wilcock. .  2nd. Cambridge University Press. 1994: 170  [2010-05-07]. ISBN 0521446694. （原始内容存档于2021-01-16）.
↑  David Johnson. . . Cambridge University Press. 2004: 48 ff  [2010-05-07]. ISBN 0521841216. （原始内容存档于2020-02-24）.
↑  Five characteristics of the orogenic cycle are listed by Robert J. Twiss, Eldridge M. Moores. .  2nd. Macmillan. 1992: 493  [2010-05-07]. ISBN 0716722526. （原始内容存档于2020-03-11）.
↑  N. H. Woodcock, Robin A. Strachan. . . : 187 ff  [2010-05-07]. ISBN 0632036567. （原始内容存档于2020-03-05）.
↑  Olivier Merle. . . Springer. 1998: 1 ff  [2010-05-07]. ISBN 0792348796. （原始内容存档于2020-02-27）.
↑  For example, see Patrick L Osborne. . Cambridge University Press. 2000: 11  [2010-05-07]. ISBN 0521645239. （原始内容存档于2020-02-26）. Continental drift and plate tectonics help to explain both the similarities and the differences in the distribution of plants and animals over the continents  and John C Briggs. . Elsevier. 1987: 131  [2010-05-07]. ISBN 0444427430. （原始内容存档于2020-02-15）. It will not be possible to construct a thorough account of the history of the southern hemisphere without the evidence from both the biological and the earth sciences
↑  Paul D. Lowman. . . Cambridge University Press. 2002: 286–287  [2010-05-07]. ISBN 0521890624. （原始内容存档于2016-06-03）.
↑  Seema Sharma. . . Anmol Publications PVT. LTD. 2005: 30 ff  [2010-05-07]. ISBN 8126124423. （原始内容存档于2013-06-10）.
↑  Richard J. Huggett.  2nd. Routledge. 2007: 104  [2010-05-07]. ISBN 0415390842. （原始内容存档于2020-02-29）.
↑  Gerhard Einsele.  2nd. Springer. 2000: 453  [2010-05-07]. ISBN 354066193X. （原始内容存档于2020-01-25）. Without denudation, even relatively low uplift rates as characteristic of epeirogenetic movements (e.g. 20m/MA) would generate highly elevated regions in geological time periods.
↑  Peter J Coney. . Geological Society of America Bulletin. 1970, 81 (3): 739–748. doi:10.1130/0016-7606(1970)81[739:TGCATN]2.0.CO;2.
1 2  Lee, C.-T.  (PDF). Science. 2000, 289: 1912. doi:10.1126/science.289.5486.1912. （原始内容 (PDF)存档于2011-06-15）.
↑  John Gerrard. . MIT Press. 1990: 9  [2010-05-07]. ISBN 0262071282. （原始内容存档于2020-03-05）.
↑  Manley, Curtis R. . Geology. 2000, 28: 811. doi:10.1130/0091-7613(2000)28<811:TOVITS>2.0.CO;2.
↑  Arthur Holmes, Doris L. Holmes.  4rth. Taylor & Francis. 2004: 92  [2010-05-07]. ISBN 0748743812. （原始内容存档于2020-02-29）.
↑  Zwart, H. J., 1967. The duality of orogenicb elts. Geol. Mijnbouw. 46, 283-309 (referred in Pitcher 1979)
↑  W.S. Pitcher, The nature, ascent and emplacement of granitic magmas, Journal of the Geological Society 1979; v. 136; p. 627-662