Plate Motions Around the Red Sea Since the Early Oligocene

  • Antonio SchettinoEmail author
  • Chiara Macchiavelli
  • Najeeb M. A. Rasul


The Red Sea represents a very young oceanic basin that formed between Nubia and Arabia since chron C3 (~4.6 Ma). The rifting phase started at ~30 Ma (early Oligocene) and can be represented by two kinematic stages, characterized by distinct directions of extension and different duration. Deformation associated with rifting was accommodated through the reactivation of the inherited Proterozoic structures. We show that the first stage was characterized by the northward motion of the Arabian plate with respect to Africa, accompanied by a pattern of deformation that included N–S oriented strike–slip faults and normal faults having E–W strike. During this stage, extension was mainly accommodated by the formation of pull–apart basins. Starting from ~27 Ma (late Oligocene), the extension axes changed dramatically and acquired the modern NE–SW pattern, which was conserved until the early Pliocene in the southern Red Sea and is still active in the northern region. In this time interval, an inherited system of NW–SE structures was reactivated as normal faults accommodating NE–SW extension, while NE–SW Proterozoic structures were reactivated as transfer strike–slip faults. Although no changes in the directions of extension are observed during this interval, two significant tectonic events occurred around 14 Ma and at 1.77 Ma. During the Langhian, two intervening microplates formed between Nubia and Arabia; the Danakil and Sinai microplates, whose motion determined the formation of the Afar Depression and the Gulf of Aqaba, respectively. Finally, starting from the Pleistocene, ongoing collision of Arabia with Eurasia along the Zagros mountains resulted into a dramatic slowdown in the Red Sea opening rates.



This work was funded by the Italian Ministry of University and Scientific Research, PRIN prot. 20125JKANY, and by the Saudi Geological Survey (SGS). The authors are grateful to the SGS personnel who helped them in surveying the area and to the SGS drivers who showed great professionality in their difficult work. Finally, the authors thank four anonymous reviewers for their accurate reviews and useful suggestions that considerably improved this paper.


  1. Agard P, Omrani J, Jolivet L, Mouthereau F (2005) Convergence history across Zagros (Iran): constraints from collisional and earlier deformation. Int J Earth Sci 94(3):401–419CrossRefGoogle Scholar
  2. Al-Damegh K, Sandvol E, Barazangi M (2005) Crustal structure of the Arabian plate: new constraints from the analysis of teleseismic receiver functions. Earth Planet Sci Lett 231(3):177–196CrossRefGoogle Scholar
  3. ArRajehi A, McClusky S, Reilinger R, Daoud M, Alchalbi A, Ergintav S, Gomez F, Sholan J, Bou-Rabee F, Ogubazghi G, Haileab B, Fisseha S, Asfaw L, Mahmoud S, Rayan A, Bendik R, Kogan L (2010) Geodetic constraints on present-day motion of the Arabian Plate: implications for Red Sea and Gulf of Aden rifting. Tectonics 29:TC3011.
  4. Bonini M, Corti G, Innocenti F, Manetti P, Mazzarini F, Abebe T, Pecskay Z (2005) Evolution of the Main Ethiopian Rift in the frame of Afar and Kenya rifts propagation. Tectonics 24(1):TC1007. Scholar
  5. Bosworth W, Huchon P, McClay K (2005) The Red Sea and Gulf of Aden basins. J Afr Earth Sci 43(1):334–378CrossRefGoogle Scholar
  6. Brune S, Williams SE, Butterworth NP, Müller RD (2016) Abrupt plate accelerations shape rifted continental margins. Nature 536(7615):201–204CrossRefGoogle Scholar
  7. Cande SC, Kent DV (1995) Revised calibration of the geomagnetic polarity timescale for the late Cretaceous and Cenozoic. J Geophys Res 100(B4):6093–6095CrossRefGoogle Scholar
  8. Chu D, Gordon G (1998) Current plate motions across the Red Sea. Geophys J Int 135:313–328CrossRefGoogle Scholar
  9. Cochran JR (1983) A model for development of Red Sea. Am Assoc Petrol Geol Bull 67(1):41–69Google Scholar
  10. Corti G (2009) Continental rift evolution: from rift initiation to incipient break-up in the Main Ethiopian Rift, East Africa. Earth Sci Rev 96(1):1–53CrossRefGoogle Scholar
  11. d’Acremont E, Leroy S, Beslier M-O, Bellahsen N, Fournier M, Robin C, Maia M, Gente P (2005) Structure and evolution of the eastern Gulf of Aden conjugate margins from seismic reflection data. Geophys J Int 160:869–890. Scholar
  12. DeMets C, Merkouriev S (2016) High-resolution estimates of Nubia-Somalia plate motion since 20 Ma from reconstructions of the Southwest Indian Ridge, Red Sea and Gulf of Aden. Geophys J Int 207(1):317–332. Scholar
  13. Fournier M, Chamot-Rooke N, Petit C, Huchon P, Al-Kathiri A, Audin L, Beslier M-O, d’Acremont E, Fabbri O, Fleury J-M, Khanbari K, Lepvrier C, Leroy S, Maillot B, Merkouriev S (2010) Arabia-Somalia plate kinematics, evolution of the Aden-Owen-Carlsberg triple junction, and opening of the Gulf of Aden. J Geophys Res 115:B04102. Scholar
  14. Ghebreab W (1998) Tectonics of the Red Sea region reassessed. Earth-Sci Rev 45(1):1–44CrossRefGoogle Scholar
  15. Hansen SE, Rodgers AJ, Schwartz SY, Al-Amri AM (2007) Imaging ruptured lithosphere beneath the Red Sea and Arabian Peninsula. Earth Planet Sci Lett 259(3):256–265CrossRefGoogle Scholar
  16. Joffe S, Garfunkel Z (1987) Plate kinematics of the circum Red Sea—a re-evaluation. Tectonophysics 141(1):5–22CrossRefGoogle Scholar
  17. Le Pichon X, Francheteau J (1978) A plate-tectonic analysis of the Red Sea-Gulf of Aden area. Tectonophysics 46:369–406CrossRefGoogle Scholar
  18. Le Pichon XT, Gaulier JM (1988) The rotation of Arabia and the Levant fault system. Tectonophysics 153(1):271–294CrossRefGoogle Scholar
  19. Leroy S, Lucazeau F, D’Acremont E, Watremez L, Autin J, Rouzo S, Bellahsen N, Tiberi C, Ebinger C, Beslier M-O, Perrot J, Razin P, Rolandone F, Sloan H, Stuart G, Lazki AA, Al-Toubi K, Bache F, Bonneville A, Goutorbe B, Huchon P, Unternehr P, Khanbari K (2010) Contrasted styles of rifting in the eastern Gulf of Aden: a combined wide-angle, multichannel seismic, and heat flow survey. Geochem Geophys Geosys 11(7):Q07004. Scholar
  20. Leroy S, Razin P, Autin J, Bache F, d’Acremont E, Watremez L, Robinet J, Baurion C, Denèle Y, Bellahsen N, Lucazeau F, Rolandone F, Rouzo S, Serra Kiel J, Robin C, Guillocheau F, Tiberi C, Basuyau C, Beslier M-O, Ebinger C, Stuart G, Abdulhakim A, Khanbari K, Al Ganad I, de Clarens P, Unternehr P, Al Toubi K, Al Lazki K (2012) From rifting to oceanic spreading in the Gulf of Aden: a synthesis. Arab J Geosci 5:859–901. Scholar
  21. Makris J, Rihm R (1991) Shear-controlled evolution of the Red Sea: pull apart model. Tectonophysics 198(2):441–466CrossRefGoogle Scholar
  22. McKenzie DP, Davies D, Molnar P (1970) Plate tectonics of the Red Sea and East Africa. Nature 226(5242):243–248CrossRefGoogle Scholar
  23. Mouthereau F, Tensi J, Bellahsen N, Lacombe O, de Boisgrollier T, Kargar S (2007) Tertiary sequence of deformation in a thin-skinned/thick-skinned collision belt: the Zagros Folded Belt (Fars, Iran). Tectonics 26:TC5006. Scholar
  24. Nuriel P, Weinberger R, Kylander-Clark ARC, Hacker BR, Craddock JP (2017) The onset of the Dead Sea transform based on calcite age-strain analyses. Geology 45(7):587–590CrossRefGoogle Scholar
  25. Pik R, Marty B, Carignan J, Yirgu G, Ayalew T (2008) Timing of East African Rift development in southern Ethiopia: implication for mantle plume activity and evolution of topography. Geology 36(2):167–170CrossRefGoogle Scholar
  26. Reilinger R, McClusky S (2011) Nubia-Arabia-Eurasia plate motions and the dynamics of Mediterranean and Middle East tectonics. Geophys J Int 186:971–979CrossRefGoogle Scholar
  27. Salem A, Green C, Campbell S, Fairhead JD, Cascone L, Moorhead L (2013) Moho depth and sediment thickness estimation beneath the Red Sea derived from satellite and terrestrial gravity data. Geophysics 78(5):G89–G101CrossRefGoogle Scholar
  28. Salerno VM, Capitanio FA, Farrington RJ, Riel N (2016) The role of long-term rifting history on modes of continental lithosphere extension. J Geophys Res 121. Scholar
  29. Schettino A (2014) Quantitative plate tectonics. Springer, Berlin, 403 p. ISBN 978-3-319-09134-1Google Scholar
  30. Schettino A, Scotese CR (2005) Apparent polar wander paths for the major continents (200 Ma—present day): a paleomagnetic reference frame for global plate tectonic reconstructions. Geophys J Int 163(2):727–759CrossRefGoogle Scholar
  31. Schettino A, Turco E (2006) Plate kinematics of the Western Mediterranean region during the Oligocene and early Miocene. Geophys J Int 166(3):1398–1423CrossRefGoogle Scholar
  32. Schettino A, Turco E (2011) Tectonic history of the western Tethys since the late Triassic. Geol Soc Am Bull 123(1/2):89–105CrossRefGoogle Scholar
  33. Schettino A, Macchiavelli C, Pierantoni PP, Zanoni D, Rasul N (2016) Recent kinematics of the tectonic plates surrounding the Red Sea and Gulf of Aden. Geophys J Int 207:457–480. Scholar
  34. Sultan M, Becker R, Arvidson RE, Shore P, Stern RJ, El Alfy Z, Guinness EA (1992) Nature of the Red Sea crust: a controversy revisited. Geology 20(7):593–596CrossRefGoogle Scholar
  35. Sultan M, Becker R, Arvidson RE, Shore P, Stern RJ, El Alfy Z, Attia RI (1993) New constraints on Red Sea rifting from correlations of Arabian and Nubian Neoproterozoic outcrops. Tectonics 12(6):1303–1319CrossRefGoogle Scholar
  36. van Wijk JW, Cloetingh SAPL (2002) Basin migration caused by slow lithospheric extension. Earth Planet Sci Lett 198:275–288CrossRefGoogle Scholar
  37. Wolfenden E, Ebinger C, Yirgu G, Deino A, Ayalew D (2004) Evolution of the northern Main Ethiopian rift: birth of a triple junction. Earth Planet Sci Lett 224(1):213–228CrossRefGoogle Scholar
  38. Younes AI, McClay KR (2002) Development of accommodation zones in the Gulf of Suez-Red Sea rift, Egypt. Am Assoc Petrol Geol Bull 86:1003–1026Google Scholar

Copyright information

© Springer Nature Switzerland AG 2019

Authors and Affiliations

  • Antonio Schettino
    • 1
    Email author
  • Chiara Macchiavelli
    • 2
  • Najeeb M. A. Rasul
    • 3
  1. 1.School of Science and Technology – Geology DivisionUniversity of CamerinoCamerinoItaly
  2. 2.Institute of Earth Sciences Jaume AlmeraICTJA-CSIC, Lluis Sole I Sabaris S/NBarcelonaSpain
  3. 3.Center for Marine GeologySaudi Geological SurveyJeddahSaudi Arabia

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