墨西拿鹽度危機
參考文獻

↑  Manzi, Vinicio, et a.2020. The Messinian salinity crisis in the Adriatic foredeep: Evolution of the largest evaporitic marginal basin in the Mediterranean. Marine and Petroleum Geology Vol. 115
↑  Gargani J.; Rigollet C. (2007). "Mediterranean Sea level variations during the Messinian Salinity Crisis". Geophysical Research Letters. 34 (10): L10405
↑  Gargani J, Rigollet C. . Geophysical Research Letters. 2007, 34 (L10405): L10405. Bibcode:2007GeoRL..3410405G. S2CID 128771539. doi:10.1029/2007GL029885 .
↑  van Dijk, J.P., Barberis, A., Cantarella, G., and Massa, E. (1998); Central Mediterranean Messinian basin evolution. Tectono-eustasy or eustato-tectonics? Annales Tectonicae, 12, n. 1-2, 7-27.
↑  Gargani J, Rigollet C (2007). "Mediterranean Sea level variations during the Messinian Salinity Crisis". Geophysical Research Letters. 34 (L10405): L10405. Bibcode:2007GeoRL..3410405G
↑  van Dijk, J.P., Barberis, A., Cantarella, G., and Massa, E. (1998); Central Mediterranean Messinian basin evolution. Tectono-eustasy or eustato-tectonics? Annales Tectonicae, 12, n. 1-2, 7-27
↑  Weijermars, Ruud (May 1988). "Neogene tectonics in the Western Mediterranean may have caused the Messinian salinity crisis and an associated glacial event". Tectonophysics. 148 (3–4): 211–219
↑  van Dijk J.P., Okkes F.W.M. (1991). "Neogene tectonostratigraphy and kinematics of Calabrian Basins. implications for the geodynamics of the Central Mediterranean". Tectonophysics. 196 (1–2): 23–60
↑  Lonergan, Lidia; White, Nicky (June 1997). "Origin of the Betic-Rif mountain belt". Tectonics. 16 (3): 504–522
↑   Platt, J. P.; Vissers, R.L.M. (1989). "Extensional collapse of thickened continental lithosphere: A working hypothesis for the Alboran Sea and Gibraltar arc". Geology. 17 (6): 540
↑  Jackson, J.A.; Austrheim, H.; McKenzie, D.; Priestley, K. (2004). "Metastability, mechanical strength, and the support of mountain belts". Geology. 32 (7): 625
↑  van Dijk J.P., Okkes F.W.M. . Tectonophysics. 1991, 196 (1–2): 23–60. Bibcode:1991Tectp.196...23V. doi:10.1016/0040-1951(91)90288-4.
↑  Lonergan, Lidia; White, Nicky. . Tectonics. June 1997, 16 (3): 504–522. Bibcode:1997Tecto..16..504L. doi:10.1029/96TC03937. hdl:10044/1/21686 .
↑  Sonnenfeld, Peter,. 2015.The Significance of Upper Miocene (Messinian) Evaporites in the Mediterranean Sea. The Journal of Geology. Vol. 83, No. 3  P. 287-311
↑  Cunliffe, Sir Barry. . Oxford University Press. 2017-09-29: 56  [2021-10-04]. ISBN 978-0-19-107534-6. （原始内容存档于2021-10-12） （英语）. the remnant Tethys became joined to the Atlantic, roughly along the line of what was to become the Strait of Gibraltar. About 5.96 million years ago this gap closed, initiating what is known as the Messinian Salinity Crisis, which lasted for more than half a million years before the Atlantic was reunited once more with the Mediterranean.
↑  Gargani J.; Rigollet C. . Geophysical Research Letters. 2007, 34 (10): L10405. Bibcode:2007GeoRL..3410405G. S2CID 128771539. doi:10.1029/2007gl029885 .
↑  Schreiber, C. S., et al. 1976. Depositional environments of Upper Miocene (Messinian) evaporite deposits of the Sicilian Basin. Sedimentology, Vol. 23 Issue 6. p.729-760
↑  Lofi, Johanna, et al. 2011. Seismic Atlas of the Messinian Salinity Crisis markers in the Mediterranean and Black Seas. Commission for the Geological Map of the World & Memories of the French Geological Society ISBN 2-85363-097-8
↑   Mailland, Agnes, et al., 2020. New onshore/offshore evidence of the Messinian Erosion Surface from key areas: The Ibiza-Balearic Promontory and the Orosei-Eastern Sardinian margin.Bulletin de la Société Géologique de France。 Vol。191。https://doi.org/10.1051/bsgf/2020007
↑  Schreiber, C. S., et al. 1976. Depositional environments of Upper Miocene (Messinian) evaporite deposits of the Sicilian Basin. Sedimentology, Vol. 23 Issue 6. p.729-760,
1 2  Madof, A. S., etal., 2019. Discovery of vast fluvial deposits provides evidence for drawdown during the late Miocene Messinian salinity crisis. Geology Vol. 47, P. 171–174
↑  Clauzon, Georges; Suc, Jean-Pierre; Gautier, François; Berger, André; Loutre, Marie-France. . Geology. 1996, 24 (4): 363. Bibcode:1996Geo....24..363C. doi:10.1130/0091-7613(1996)024<0363:AIOTMS>2.3.CO;2.
↑  Lecture 17: Mediterranean 的存檔，存档日期2010-05-23.
↑  Warren, John K. . Birkhäuser. 2006: 147  [2016-12-15]. ISBN 978-3-540-26011-0. （原始内容存档于2021-10-04）.
↑  . Biot Report 403. September 21, 2006  [2021-10-04]. （原始内容存档于2013-06-30）.
↑  https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2007GL032494 （页面存档备份，存于）, Geophysical Research Letters, Evaporite accumulation during the Messinian Salinity Crisis: The Suez Rift case, by Julien Gargani, Isabelle Moretti, Jean Letouzey, First published: 16 January 2008, https://doi.org/10.1029/2007GL032494
↑  A. Simmons. . Geoarchaeology. 2000, 15 (4): 379–381. doi:10.1002/(SICI)1520-6548(200004)15:4<379::AID-GEA7>3.0.CO;2-E.
↑  Gargani J.; Rigollet C; Scarselli S. . Bull. Soc. Géol. Fr. 2010, 181: 19–26. doi:10.2113/gssgfbull.181.1.19.
↑  Gargani J. . Quaternary International. 2004, 121: 13–22. Bibcode:2004QuInt.121...13G. doi:10.1016/j.quaint.2004.01.020.
↑  Petronio, C.  (PDF). Ibex. 1995, 3: 53–55  [2008-08-23]. （原始内容 (PDF)存档于2008-09-12）.
↑  Gargani J.; Rigollet C; Scarselli S. . Bull. Soc. Géol. Fr. 2010, 181: 19–26. doi:10.2113/gssgfbull.181.1.19.
↑  Gargani J. . Quaternary International. 2004, 121 (1): 13–22. Bibcode:2004QuInt.121...13G. doi:10.1016/j.quaint.2004.01.020.
↑  Warren, J.K. . Birkhäuser. 2006: 352  [2016-12-15]. ISBN 978-3-540-26011-0. （原始内容存档于2021-11-06）.
↑  Druckman, Y., et al ., 1995.The buried Afiq Canyon (Eastern Mediterranean, Israel): a case study of a Tertiary submarine canyon exposed in Late Messinian times. Marine Geology Volume 123, Issues 3–4, April 1995, Pages 167-185)
↑   Barr, F. T.  and Walker, B. R. 2004. LATE TERTIARY CHANNEL SYSTEM IN NORTHERN LIBYA AND ITS IMPLICATIONS ON MEDITERRANEAN SEA LEVEL CHANGES. in Petroleum Geology of Libya, ed. Hallett, Don.  Publ. Elservier. ISBN 50525-3
↑  Wade, B.S.; Brown P.R.  (PDF). Palaeogeography, Palaeoclimatology, Palaeoecology. 2006, 233 (3–4): 271–286  [2016-12-15]. doi:10.1016/j.palaeo.2005.10.007. （原始内容存档 (PDF)于2016-03-03）.