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From rifting to oceanic spreading in the Gulf of Aden: A synthesis

  • Sylvie Leroy
  • Philippe Razin
  • Julia Autin
  • François Bache
  • Elia d’Acremont
  • Louise Watremez
  • Jérémy Robinet
  • Céline Baurion
  • Yoann Denèle
  • Nicolas Bellahsen
  • Francis Lucazeau
  • Frédérique Rolandone
  • Stéphane Rouzo
  • Josep Serra Kiel
  • Cécile Robin
  • François Guillocheau
  • Christel Tiberi
  • Clémence Basuyau
  • Marie-Odile Beslier
  • Cynthia Ebinger
  • Graham Stuart
  • Abdulhakim Ahmed
  • Khaled Khanbari
  • Ismael Al- Ganad
  • Philippe de Clarens
  • Patrick Unternehr
  • Khalfan Al- Toubi
  • Ali Al- Lazki
Conference paper
Part of the Frontiers in Earth Sciences book series (FRONTIERS)

Abstract

We present here a synthesis of the evolution of rifted continental margin systems in the Gulf of Aden. These margins are volcanic to the West of the Gulf of Aden, where they are influenced by the Afar hotspot, and non-volcanic East of longitude 46°E. The combined use of magnetics, gravity, seismic reflection, field observations (tectonic and sedimentological) and oil-well data allowed us to obtain better constraints on the timing of continental rifting and seafloor spreading. From the Permo-Triassic to the Oligocene, the Arabian-African plate was subject to distributed extension, probably due, at least from the Cretaceous, to tensile stresses related to the subduction of the Tethysian slab in the north. In Late Eocene, 35 Ma ago, rifting started to localise along the future area of continental breakup. Initially guided by the inherited basins, continental rifting then occurred synchronously over the entire gulf before becoming localised on the northern and southern borders of the inherited grabens, in the direction of the Afar hotspot. In the areas with non-volcanic margins (in the East), the faults marking the end of rifting trend parallel to the inherited grabens. Only the transfer faults cross-cut the inherited grabens, and some of these faults later developed into transform faults. The most important of these transform faults follow a Precambrian trend. Volcanic margins were formed in the West of the Gulf, up to the Guban graben in the south-east and as far as the southern boundary of the Bahlaf graben in the North-East. Seaward dipping reflectors (SDRs) can be observed on many oil-industry seismic profiles. The influence of the hotspot during rifting was concentrated on the western part of the gulf. Therefore, it seems that the western domain was uplifted and eroded at the onset of rifting, while the eastern domain was characterised by more continuous sedimentation. The phase of distributed deformation was followed by a phase of strain localisation during the final rifting stage, just before formation of the Ocean-Continent Transition (OCT), in the most distal graben (DIM graben). About 20 Ma ago, at the time of the continental break-up, the emplacement of the OCT started in the east with exhumation of the subcontinental mantle. Farther west, the system was heated up by the strong influence of the Afar hotspot, which led to breakup with much less extension. In the Gulf of Aden (s.str), up to the Shukra El Sheik fracture zone, oceanic spreading started 17.6 Ma ago. West of this fracture zone, oceanic accretion started 10 Ma ago, and 2 Ma ago in the Gulf of Tadjoura. Post-rift deformation of the eastern margins of the Gulf of Aden can be seen in the distal and proximal domains. Indeed, the substantial post-rift uplift of these margins could be associated with either the continental break-up, or activity of the Afar hotspot and related volcanic/magmatic activity. Uplift of the northern proximal margin was still active (e.g. stepped beach rocks exposed at 60 m of 2 Ma; 30 m of 35,200 y; 10 and 2 m) and active volcanoes can be inferred at depths of between 70 and 200 km beneath the margin (at 5–10 km distance from the coast). On the distal margin, heat flow measurements show a high value that are associated with post-rift volcanic activity and the development of a volcano (with flows and sills) shortly after the formation of the OCT. The Afar hotspot is therefore important for several reasons. It allows the localisation of deformation along the Red Sea/Aden system and the rapid opening of the Gulf after the continental break-up; its influence also seems to persist during the post-rift period.

Keywords

Continental Rift Arabian Plate Oceanic Spreading Dammam Formation Rift Continental Margin 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

Notes

Acknowledgments

This study is a contribution due to GDR Marges, Actions Marges, ANR YOCMAL, INSU-DYETI, CNRS-PICS Oman and CNRS-PICS Yemen. We thank Philippe Patriat for stimulating discussions and also Nadine Ellouz-Zimmermann. We are grateful to the Ministry of Commerce and Industry, Directorate of Minerals of Muscat, Ministry of Oil and Gas, GSMRB, French Embassies in Sana’a and in Muscat for their support during the project.

References

  1. Agard P, Omrani J, Jolivet L, Mouthereau F (2005) Convergence history across Zagros, Iran; constraints from collisional and earlier deformation. Geol Rundsch Int J Earth Sci 94(3):401–419 (1999 Print)CrossRefGoogle Scholar
  2. Agostini A, Bonini M, Corti G, Sani F, Mazzarini F (2011) Fault architecture in the main Ethiopian rift and comparison with experimental models: Implications for rift evolution and Nubia-Somalia kinematics. Earth Planet Sci Lett 301(3–4):479–492. doi: 10.1016/j.epsl.2010.11.024 CrossRefGoogle Scholar
  3. Aharon P (1994) Geology and biology of modern and ancient submarine hydrocarbon seeps and vents: an introduction. Geo-Mar Lett 14(2):69–73. doi: 10.1007/bf01203716 CrossRefGoogle Scholar
  4. Al-Riyami O (2007) Receiver function analysis. University, LeedsGoogle Scholar
  5. Audin L et al (2004) Palaeomagnetism and K–Ar and 40Ar/39Ar ages in the Ali Sabieh area (Republic of Djibouti and Ethiopia): constraints on the mechanism of Aden ridge propagation onto southeastern Afar during the last 10 Myr. Geophys J Int 158:327–345. doi: 10.1111/j.1365-246X.2004.02286.x Google Scholar
  6. Autin J (2008) Déchirure continentale et segmentation du golfe d’Aden oriental en contexte de rifting oblique. University Paris 06, ParisGoogle Scholar
  7. Autin J, Bellahsen N, Husson L, Beslier M-O, Leroy S, d’Acremont E (2010a) Analogue models of oblique rifting in a cold lithosphere. Tectonics, vol 29 (TC6016). doi: 10.1029/2010TC002671
  8. Autin J, Leroy S, Beslier MO, d’Acremont E, Razin P, Ribodetti A, Bellahsen N, Robin C, Al-Toubi K (2010b) Continental break-up history of a deep magma-poor margin from seismic reflection data (Northeastern Gulf of Aden margin, offshore Oman). Geophys J Int 180:501–519CrossRefGoogle Scholar
  9. Bache F, Leroy S, Baurion C, Robinet J, Gorini C, Lucazeau F, Razin P, d’Acremont E, Al-Toubi K (2011) Post-rift uplift of the Dhofar margin (Gulf of Aden). Terra Nova 23(1):11–18. doi: 10.1111/j.1365-3121.2010.00975.x CrossRefGoogle Scholar
  10. Basuyau C (2006) Determination d'interfaces crustales et mantelliques par inversion des fonctions recepteur, application à la region du Dhofar (Oman). MsC, Univ, Paris 6Google Scholar
  11. Basuyau C, Tiberi C, Leroy S, Stuart G, Al-Lazki A, Al-Toubi K, Ebinger C (2010) Evidence of partial melting beneath a continental margin: case of Dhofar, in the Northern Gulf of Aden (Sultanante of Oman). Geophys J Int 180:520–534CrossRefGoogle Scholar
  12. Bellahsen N, Autin J, Leroy S, d’Acremont E, Beslier M-O, Husson L, Al-Toubi K (2009) How and when did a strong thinning occur in the Gulf of Aden ? A discussion from field, geophysical data and analogue models. In: Paper presented at the fall meeting, San FranciscoGoogle Scholar
  13. Bellahsen N, Faccenna C, Funiciello F, Daniel J-M, Jolivet L (2003) Why did Arabia separate from Africa? Insights from 3-D laboratory experiments. Earth Planet Sci Lett 216:365–381CrossRefGoogle Scholar
  14. Bellahsen N, Fournier M, d’Acremont E, Leroy S, Daniel J-M (2006) Fault reactivation and rift localization: Northeastern Gulf of Aden margin. Tectonics, vol 25, pp 1–14. doi: 10.1029/2004TC001626
  15. Beydoun ZR (1998) Arabian plate oil and gas; Why so rich and so prolific? Episodes 21(2):74–81Google Scholar
  16. Beydoun ZR, Bichan HR (1969) The geology of Socotra Island, Gulf of Aden. Quat J 125:413–446Google Scholar
  17. Birse ACR, Bott WF, Morrison J, Samuel MA (1997) The Mesozoic and early tertiary tectonic evolution of the Socotra area, eastern Gulf of Aden, Yemen. Marine Pet Geol 14(6):675–684CrossRefGoogle Scholar
  18. Blaich OA, Faleide JI, Tsikalas F (2011) Crustal breakup and continent-ocean transition at South Atlantic conjugate margins. J Geophys Res 116 (B1):B01402. doi: 10.1029/2010jb007686
  19. Borowski WS, Paull CK, Ussler W (1999) Global and local variations of interstitial sulfate gradients in deep-water, continental margin sediments: sensitivity to underlying methane and gas hydrates. Mar Geol 159(1–4):131–154. doi: 10.1016/s0025-3227(99)00004-3 CrossRefGoogle Scholar
  20. Bosworth W, Huchon P, McClay K (2005) The Red Sea and Gulf of Aden Basins. J Afr Earth Sc 43:334–378CrossRefGoogle Scholar
  21. Bott MHP (1982) The mechanism of continental splitting. Tectonophysics 81:301–309CrossRefGoogle Scholar
  22. Bott WF, Smith BA, Oakes G, Sikander AH, Ibrahim AI (1992) The tectonic framework and regional hydrocarbon, prospectivity of the Gulf of Aden. J petrol Geol 15:211–243CrossRefGoogle Scholar
  23. Brannan J, Gerdes KD, Newth IR (1997) Tectono-stratigraphic development of the Qamar basin, eastern Yemen. Mar Pet Geol 14(6):701–730 (IN707-IN712)CrossRefGoogle Scholar
  24. Brew G, Barazangi M, Al-Maleh K, Sawaf T (2001) Tectonic and geologic evolution of Syria. Geo Arabia 6(3):573–616Google Scholar
  25. Buck WR (2004) Consequences of asthenospheric variability on continental rifting. In: Karner G, Taylor B, Driscoll N, Kohlstedt L (eds) Rheology and deformation of the Lithosphere at continental margins. Columbia University Press, New York, pp 1–30Google Scholar
  26. Bunter MAG, Debretsion T, Woldegiorgis L (1998) New developments in the pre-rift prospectivity of the Eritrean Red Sea. J Pet Geol 21(4):373–400CrossRefGoogle Scholar
  27. Bunter MAG, Magid AEMA (1989) The sudanese red sea: 1 New developments in stratigraphy and petroleum-geological evolution. J Pet Geol 12(2):145–166. doi: 10.1111/j.1747-5457.1989.tb00230.x CrossRefGoogle Scholar
  28. Chaubey AK, Dyment J, Bhattacharya GC, Royer J-Y, Srinivas K, Yatheesh V (2002) Paleogene magnetic isochrons and paleo-propagators in the Arabian and Eastern Somali basins, NW Indian Ocean. In: Clift PD, Kroon D, Gaedicke C, Craig J (eds) The tectonic and climatic evolution of the Arabian Sea Region, vol 195., Geol SocSpecial Publications, London, pp 71–85Google Scholar
  29. Cloetingh S, van Wees JD, van der Beek PA, Spadini G (1995) Role of pre-rift rheology in kinematics of extensional basin formation: constraints from thermo mechanical models of Mediterranean and intracratonic basins. Mar Pet Geol 12(8):793–807. doi: 10.1016/0264-8172(95)98848-y CrossRefGoogle Scholar
  30. Corti G (2008) Control of rift obliquity on the evolution and segmentation of the main Ethiopian rift. Nat Geosci 1(4):258–262. doi:http://www.nature.com/ngeo/journal/v1/n4/suppinfo/ngeo160_S1.html Google Scholar
  31. Courtillot V, Jaupart C, Manighetti I, Tapponnier P, Bess J (1999) On causal links between flood basalts and continental breakup. Earth Planet Sci Lett 166:177–195CrossRefGoogle Scholar
  32. Cowie PA, Underhill JR, Behn MD, Lin J, Gill CE (2005) Spatio-temporal evolution of strain accumulation derived from multi-scale observations of late Jurassic rifting in the northern North Sea: a critical test of models for lithospheric extension. Earth Planet Sci Lett 234(3–4):401–419CrossRefGoogle Scholar
  33. d’Acremont E, Leroy S, Beslier MO, 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 160:869–890CrossRefGoogle Scholar
  34. d’Acremont E, Leroy S, Burov Evgenii B (2003) Numerical modelling of a mantle plume; the plume head-lithosphere interaction in the formation of an oceanic large igneous province. Earth Planet Sci Lett 206(3–4):379–396CrossRefGoogle Scholar
  35. d’Acremont E, Leroy S, Maia M, Patriat P, Beslier MO, Bellahsen N, Fournier M, Gente P (2006) Structure and evolution of the eastern Gulf of Aden: insights from magnetic and gravity data (Encens-Sheba/MD117 cruise). Geophys J Int 165:786–803CrossRefGoogle Scholar
  36. d’Acremont E, Leroy S, Maia M, Gente P, Autin J (2010) Volcanism, jump and propagation on the Sheba Ridge, eastern Gulf of Aden: segmentation evolution and implications for accretion processes. Geophys J Int 180:535–551CrossRefGoogle Scholar
  37. Dauteuil O, Huchon P, Quemeneur F, Souriot T (2001) Propagation of an oblique spreading center: the western Gulf of Aden. Tectonophysics 332:423–442CrossRefGoogle Scholar
  38. Denèle Y, Leroy S, Champanhet JM, Bellahsen N, Pik R (2009) Proterozoic inheritance in the Gulf of Aden: the exmaple of the Socotra Island (Yemen). In: Paper presented at the Fall meeting, San FranciscoGoogle Scholar
  39. Denèle Y, Leroy S, Pelleter E, Pik R, Talbot JY, Khanbari K (2011) The Cryogenian juvenile Arc formation and successive high-K calc-alkaline plutons intrusion of Socotra Island (Yémen). Springer VolumeGoogle Scholar
  40. Dyment J (1998) Evolution of the carlsberg ridge between 60 and 45 Ma: ridge propagation, spreading asymmetry, and the Deccan-Reunion hotspot. J Geophys Res 103(B10):24067–24084Google Scholar
  41. Ebinger CJ, Keir D, Ayele A, Calais E, Wright TJ, Belachew M, Hammond JOS, Campbell E, Buck WR (2008) Capturing magma intrusion and faulting processes during continental rupture: seismicity of the Dabbahu (Afar) rift. Geophys J Int 174(3):1138–1152. doi: 10.1111/j.1365-246X.2008.03877.x CrossRefGoogle Scholar
  42. Edwards RA, Minshull TA, White RS (2000) Extension across the Indian-Arabian plate boundary: the Murray Ridge. Geophys J Int 142:461–477CrossRefGoogle Scholar
  43. El-Shinnawi MA (1975) Planktonic foraminifera from the Miocene Globigerina Marl of Hurgada Well-134, Eastern Desert, Egypt. In: Mineras ENAdI (ed) 5th African Colloquium on Micropalaeontology, Addis Ababa, pp 199–224Google Scholar
  44. Ellis AC, Kerr HM, Cornwell CP, Williams DO (1996) A tectono-stratigraphic framework for Yemen and its implications for hydrocarbon potential. Pet Geosci 2(1):29–42CrossRefGoogle Scholar
  45. Fantozzi PL (1996) Transition from continental to oceanic rifting in the Gulf of Aden: structural evidence from field mapping in Somalia and Yemen. Tectonophysics 259(4):285–311CrossRefGoogle Scholar
  46. Fantozzi PL, Ali-Kassim M (2002) Geological mapping in northeastern Somalia (Midjiurtinia region): field evidence of the structural and paleogeographic evolution of the northern margin of the Somalian plate. J Afr Earth Sci 34:21–55CrossRefGoogle Scholar
  47. Fantozzi PL, Sgavetti M (1998) Tectonic and sedimentary evolution of the eastern Gulf of Aden continental margins: new structural and stratigraphic data from Somalia and Yemen. In: Purser BH, Bosence DWJ (eds) Sedimentation and tectonics of Rift Basins: Red Sea-Gulf of Aden. Chapman and Hall, London, pp 56–76CrossRefGoogle Scholar
  48. Fournier M, Bellahsen N, Fabbri O, Gunnell Y (2004) Oblique rifting and segmentation of the NE Gulf of Aden passive margin. Geochem Geophys Geosys 5(11):24Google Scholar
  49. 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(B4):B04102. doi: 10.1029/2008jb006257 Google Scholar
  50. Fournier M, Huchon P, Khanbari K, Leroy S (2007) Asymmetry and segmentation of passive margin in Socotra, Eastern Gulf of Aden, controlled by detachment faults ? Geochem Geophys Geosyst 8(3):Q03013. doi: 03010.01029/02006GC001318 CrossRefGoogle Scholar
  51. Fournier M, Petit C, Chamot-Rooke N, Fabbri O, Huchon P, Maillot B, Lepvrier C (2008) Do ridge–ridge-fault triple junctions exist on earth? Evidence from the Aden-Owen-Carlsberg junction in the NW Indian Ocean. Basin Research (0)Google Scholar
  52. Geoffroy L (2005) Volcanic passive margins. In: CR Geoscience, Concise review paper, vol 337, pp 1395–1408Google Scholar
  53. George R, Rogers N, Kelley S (1998) Earliest magmatism in Ethiopia: evidence for two mantle plumes in one flood basalt province. Geology 26:923–926CrossRefGoogle Scholar
  54. Gernigon L, Ringenbach Jean C, Planke S, Le Gall B (2004) Deep structures and breakup along volcanic rifted margins; insights from integrated studies along the outer Voring Basin (Norway). Mar Pet Geol 21(3):363–372CrossRefGoogle Scholar
  55. Gnos E, Immenhauser A, Peters T (1997) Late cretaceous/early tertiary convergence between the Indian and Arabian plates recorded in ophiolites and related sediments. Tectonophysics 271:1–19CrossRefGoogle Scholar
  56. Granath JW (2001) The Nogal Rift of northern Somalia: Gulf of Aden. Reactivation of a Mesozoic Rift. Editions du Museum, Paris, FranceGoogle Scholar
  57. Hancock PL, Al Kadhi A, at Sha NA (1984) Regional joint sets in the Arabian platform as indicators of intraplate processes. Tectonics 3(1):27–43CrossRefGoogle Scholar
  58. Hill RI (1991) Starting plumes and continental break-up. Earth Planet Sci Lett 104(2–4):398–416CrossRefGoogle Scholar
  59. Hofmann C, Courtillot V, Féraud G, Rochette P, Yirgu E, Kefeto E, Pik R (1997) Timing of the Ethiopian flood basalt event and implications for plume birth and global change. Nature 389:838–841CrossRefGoogle Scholar
  60. Hopper JR, Buck WR (1996) The effect of lower crustal flow on continental extension and passive margin formation. J Geophys Res 101(B9):20175–20194Google Scholar
  61. Hopper JR, Mutter J, Larson R, Mutter C, Buhl P, Diebold J, Alsop J, Falvey D, Williamson P, Brassil P, Lorenzo JM (1992) Magmatism and rift margin evolution: evidence from northwest Australia. Geology 20:853–857CrossRefGoogle Scholar
  62. Huchon P, Jestin F, Cantagrel JM, Gaulier JM, Kirbash SA, Gafaneh A (1991) Extensional deformation in Yemen since Oligocene and the Africa-Arabia-Somalia triple junction. Annales Tectonicae, vol 5, pp 141–163Google Scholar
  63. Huchon P, Khanbari K (2003) Rotation of the syn-rift stress field of the northern Gulf of Aden margin, Yemen. Tectonophysics 364(3–4):147–166CrossRefGoogle Scholar
  64. Hughes G, Filatoff J (1995) New biostratigraphic constraints on Saudi Arabian Red Sea pre- and syn-rift sequences. In: Al-Huseini MI (ed) Middle East petroleum geosciences, vol 94. Gulf Petrolink, Bahrein, pp 517–528Google Scholar
  65. Immenhauser A, Schreurs G, Gnos E, Oterdoom HW, Hartmann B (2000) Late Palaeozoic to Neogene geodynamic evolution of the northeastern Oman margin. Geol Mag 137(1):1–18CrossRefGoogle Scholar
  66. Jolivet L, Faccenna C (2000) Mediterranean extension and the Africa-Eurasia collision. Tectonics 19(6):1095–1106CrossRefGoogle Scholar
  67. Khanbari K (2000) Propagation d’un rift océanique: le Golfe d’Aden, Ses effets structuraux sur la marge yéménite. Université Paris-Sud, ParisGoogle Scholar
  68. Khanbari K, Huchon P (2010) Paleostress analysis of the volcanic margins of Yemen. Arabian J Geosci 3(4):529–538. doi: 10.1007/s12517-010-0164-8 CrossRefGoogle Scholar
  69. Lavier LL, Manatschal G (2006) A mechanism to thin the continental lithosphere at magma-poor margins. Nature 440:324–328CrossRefGoogle Scholar
  70. Le Métour JC, Michel JC, Béchennec F, Platel J-P, Roger J (1995) Geology and mineral wealth of the Sultanate of Oman. In: M.P.M. Geological documents. Ministry of Petroleum and Minerals, Directorate General of Minerals, p 285Google Scholar
  71. Lepvrier C, Fournier M, Bérard T, Roger J (2002) Cenozoic extension in coastal Dhofar (southern Oman): implications on the oblique rifting of the Gulf of Aden. Tectonophysics 357:279–293CrossRefGoogle Scholar
  72. Leroy S (2010) Dynamique de la rupture continentale et de l’accrétion océanique. UPMCGoogle Scholar
  73. Leroy S, d’Acremont E, Tiberi C, Basuyau C, Autin J, Lucazeau F, Sloan H (2010a) Recent off-axis volcanism in the eastern Gulf of Aden: implications for plume-ridge interaction. Earth Planet Sci Lett 293(1–2):140–153. doi: 10.1016/j.epsl.2010.02.036 CrossRefGoogle Scholar
  74. Leroy S, Gente P, The scientific shipboard party (2004) From rifting to spreading in the eastern Gulf of Aden : a geophysical survey of a young oceanic basin from margin to margin. Terra Nova 16:185–192Google Scholar
  75. 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, Al-Lazki A, Al-Toubi K, Bache F, Bonneville A, Goutorbe B, Huchon P, Unternehr P, Khanbari K (2010b) Contrasted styles of rifting in the eastern Gulf of Aden: a combined wide-angle MCS and Heat flow survey. Geochem Geophys Geosyst 11(Q07004):1–14. doi:doi: 10.1029/2009GC002963
  76. Leroy S, Lucazeau F, Razin P, Manatschal G, team. Y (2007) The ≪ Young conjugate margins laboratory ≫ project in the Gulf of Aden paper presented at the fall meeting, San FranciscoGoogle Scholar
  77. Leroy S, Mauffret A, Patriat P, de Mercier LB (2000) An alternative interpretation of the cayman trough evolution from a re identification of magnetic anomalies. Geophys J Int 141:539–557CrossRefGoogle Scholar
  78. Litak RK, Barazangi M, Beauchamp W, Seber D, Brew G, Sawaf T, Al Youssef W (1997) Mesozoic-Cenozoic evolution of the intraplate Euphrates fault system, Syria; implications for regional tectonics. J Geol Soc Lon 154(Part 4):653–666Google Scholar
  79. Lucazeau F, Leroy S, Autin J, Bonneville A, Goutorbe B, Rolandone F, d’Acremont E, Watremez L, Düsünur D, Huchon P (2009) Post-Rift Volcanism and high heat-flow at the ocean-continent transition of the Gulf of Aden. Terra Nova 21(4):285–292CrossRefGoogle Scholar
  80. Lucazeau F, Leroy S, Bonneville A, Goutorbe B, Rolandone F, d’Acremont E, Watremez L, Düsünur D, Tuchais P, Huchon P, Bellahsen N, Al-Toubi K (2008) Persistent thermal activity at the Eastern Gulf of Aden after continental break-up. Nat Geosci, pp 854–858. doi: 10.1038/ngeo359
  81. Lucazeau F, Leroy S, Rolandone F, d’Acremont E, Watremez L, Bonneville A, Goutorbe B, Düsünur D (2010) Heat-flow and hydrothermal circulations at the ocean-continent transition of the Eastern Gulf of Aden. Earth Planet Sci Lett 295(3–4):554–570. doi: 10.1016/j.epsl.2010.04.039 CrossRefGoogle Scholar
  82. Malkin BV, Shemenda AI (1991) Mechanism of rifting: considerations based on results of physical modelling and on geological and geophysical data. Tectonophysics 199:191–210CrossRefGoogle Scholar
  83. Manighetti I, Tapponnier P, Courtillot V, Gruszow S, Gillot P (1997) Propagation of rifting along the Arabia-Somalia plate boundary: the Gulfs of Aden and Tadjoura. J Geophys Res 102:2681–2710CrossRefGoogle Scholar
  84. Marquer D, Mercolli I, Peters T (1998) Early Cretaceous intra-oceanic rifting in the Proto-Indian Ocean recorded in the Masirah Ophiolite, Sultanate of Oman. Tectonophysics 292:1–16CrossRefGoogle Scholar
  85. Mercolli I, Briner AP, Frei R, Schönberg R, Nägler TF, Kramers J, Peters T (2006) Lithostratigraphy and geochronology of the Neoproterozoic crystalline basement of Salalah, Dhofar, Sultanate of Oman. Precambrian Res 145(3–4):182–206CrossRefGoogle Scholar
  86. Mittelstaedt E, Ito G, van Hunen J (2011) Repeat ridge jumps associated with plume-ridge interaction, melt transport, and ridge migration. J Geophys Res 116(B1):B01102. doi: 10.1029/2010jb007504
  87. Morgan WJ (1972) Plate motions and deep mantle convection. Geol Soc Am Mem 132:7–22Google Scholar
  88. Morley CK, Gabdi S, Seusutthiya K (2007) Fault superimposition and linkage resulting from stress changes during rifting: Examples from 3D seismic data, Phitsanulok Basin, Thailand. J Struct Geol 29(4):646–663CrossRefGoogle Scholar
  89. Moulin M, Aslanian D, Unternehr P (2010) A new starting point for the South and Equatorial Atlantic Ocean. Earth Sci Rev 98(1–2):1–37. doi: 10.1016/j.earscirev.2009.08.001 CrossRefGoogle Scholar
  90. Muntener O, Hermann J (2001) The role of lower crust and continental upper mantle during formation of non-volcanic passive margins: evidence from the Alps. Geol Soc London Spec Pub 187(1):267–288. doi: 10.1144/gsl.sp.2001.187.01.13 CrossRefGoogle Scholar
  91. Patriat P, Achache J (1984) India-Eurasia collision chronology has implications for crustal shortening and driving mechanism of plates. Nature 311(5987):615–621CrossRefGoogle Scholar
  92. Petit C, Fournier M, Gunnell Y (2007) Tectonic and climatic controls on rift escarpments: Erosion and flexural rebound of the Dhofar passive margin (Gulf of Aden, Oman). J Geophy Res, vol 112, issue B03406. doi: 10.1029/2006JB004554
  93. Platel J-P, Le Métour J, Berthiaux A, Roger J (1992a) Geological Map of Juzor Al Halaaniyaat (1/250 000). Ministry of Petroleum and MineralsGoogle Scholar
  94. Platel J-P, Roger J (1992) Geological map of Raysut (1/50 000)Google Scholar
  95. Platel JP, Roger J (1989) Evolution dynamique du Dhofar (Sultanat d’Oman) pendant le Crétacé et le Tertiaire en relation avec l’ouverture du Golfe d’Aden. Bull Soc Geol Fr 8(2):253–263Google Scholar
  96. Platel JP, Roger J, Peters T, Mercolli I, Kramers JD, Le Métour J (1992b) Geological map of salalah (1/250,000), Sultanate of Oman; sheet NE 40–09. Ministry of Petroleum and Minerals, Directorate General of Minerals, OmanGoogle Scholar
  97. Pointu A (2007) Les mouvements verticaux de la marge passive nord du Golfe d’Aden (Dhofar): causes profondes et superficielles. Phd thesis, Paris VI UniversityGoogle Scholar
  98. Purser BH, Hotzl H (1988) The sedimentary evolution of the Red Sea rift: a comparison of the northwest (Egyptian) and northeast (Saudi Arabian) margins. Tectonophysics 153(1–4):193–208. doi: 10.1016/0040-1951(88)90015-7 CrossRefGoogle Scholar
  99. Razin P, Leroy S, Robin C, Robinet J, Serra Kiel J, Bellahsen N, Grelaud C (2010) Dispositifs Tecto-Sédimentaires syn-rift et post-rift oligo-miocènes sur la marge sud du golfe d’Aden—Ile de Socotra (Yémen). In: Paper presented at the RST, Bordeaux, octobre 2010Google Scholar
  100. Roger J, Platel JP, Cavelier C, Bourdillon-de-Grisac C (1989) Données nouvelles sur la stratigraphie et l’histoire géologique du Dhofar (Sultanat d’Oman). Bull Soc Géol Fr 2:265–277Google Scholar
  101. Royer JY (2002) Paleogene plate tectonic evolution of the Arabian and eastern Somali Basins. Geol Soc Spec Pub 195:7–23CrossRefGoogle Scholar
  102. Samuel MA, Harbury N, Bott R, Ta M (1997) Field observations from the Socotran platform: their interpretation and correlation to Southern Oman. Mar Pet Geol 14(6):661–673CrossRefGoogle Scholar
  103. Scotese CR, Gahagan LM, Larson RL (1988) Plate tectonic reconstructions of the Cretaceous and Cenozoic ocean basins. Tectonophysics 155(1–4):27–48CrossRefGoogle Scholar
  104. Sengör AMC, Burke K (1978) Relative timing of rifting and volcanism on earth and its tectonic implications. Geophys Res Lett 5:419–421CrossRefGoogle Scholar
  105. Tard F, Masse P, Walgenwitz F, Gruneisen P (1991) The volcanic passive margin in the vicinity of Aden, Yemen. In: Bulletin des centres de recherches exploration-production elf-aquitaine, vol 15(1), pp 1–9Google Scholar
  106. Thomas W (2006) Tectonic inheritance at a continental margin. GSA Today 16(2):4–11. doi: 10.1130/1052-5173(2006)016<4:TIAACM>2.0.CO;2 CrossRefGoogle Scholar
  107. Thoué F, Vidal G, Gratier J-P (1997) Finite deformation and displacement fields on the southern Yemen margin using satellite images, topographic data and a restoration method. Tectonophysics 281(3):173–193CrossRefGoogle Scholar
  108. Tiberi C, Leroy S, d’Acremont E, Bellahsen N, Ebinger C, Al-Lazki A, Pointu A (2007) Crustal geometry of the northeastern Gulf of Aden passive margin: localization of the deformation inferred from receiver function analysis. Geophys J Int, vol 168, pp 1247–1260. doi: 10.1111/j.1365-246X.2006.03294.x
  109. Tommasi A, Knoll M, Vauchez A, Signorelli JW, Thoraval C, Loge R (2009) Structural reactivation in plate tectonics controlled by olivine crystal anisotropy. Nat Geosci 2(6):423–427. doi:http://www.nature.com/ngeo/journal/v2/n6/suppinfo/ngeo528_S1.html Google Scholar
  110. Tron V, Brun JP (1991) Experiments on oblique rifting in brittle–ductile systems. Tectonophysics 188:71–84CrossRefGoogle Scholar
  111. Turcotte DL, Emerman SH (1983) Mechanisms of active and passive rifting. Tectonophysics 94:39–50CrossRefGoogle Scholar
  112. van der Beek P, Andriessen P, Cloetingh S (1995) Morphotectonic evolution of rifted continental margins: Inferences from a coupled tectonic-surface processes model and fission track thermochronology. Tectonics 14(2):406–421. doi: 10.1029/94tc02445 CrossRefGoogle Scholar
  113. van Wijk JW, Cloetingh SAPL (2002) Basin migration caused by slow lithospheric extension. Earth Planet Sci Lett 198(3–4):275–288CrossRefGoogle Scholar
  114. Watchorn F, Nichols GJ, Bosence DWJ (1998) Rift-related sedimentation and stratigraphy, southern Yemen (Gulf of Aden). In: Purser B, Bosence D (eds) Sedimentation and Tectonics in the Rift Basins Red Sea-Gulf of Aden. Chapman and Hall, London, pp 165–189CrossRefGoogle Scholar
  115. Watremez L, Leroy S, Rouzo S, d’Acremont E, Unternehr P, Ebinger C, Lucazeau F, Al-Lazki A (2011) The crustal structure of the north-eastern Gulf of Aden continental margin: insights from wide-angle seismic data. Geophys J Int 184(2):575–594. doi: 10.1111/j.1365-246X.2010.04881.x CrossRefGoogle Scholar
  116. White RS, McKenzie DP (1989) Magmatism at rift zones: the generation of volcanic continental margins and flood basalts. J Geophys Res 94:7685–7730CrossRefGoogle Scholar
  117. Wolde B, Anonymous (1987) The Precambrian geology of Ethiopia and adjacent countries and its implications on the late Proterozoic evolution of East and Northeast Africa and Arabia. GeoSom, vol 87. In: International meeting; Geology of Somalia and surrounding regions; abstracts no 36Google Scholar
  118. Zeyen H, Volker F, Wehrle V, Fuchs K, Sobolev SV, Altherr R (1997) Styles of continental rifting: crust-mantle detachment and mantle plumes. Tectonophysics 278(1–4):329–352CrossRefGoogle Scholar
  119. Zhu L, Kanamori H (2000) Moho depth variation in southern California from teleseismic receiver functions. J Geophys Res 105:2969–2980CrossRefGoogle Scholar
  120. Ziegler MA (2001) Late Permian to Holocene paleofacies evolution of the Arabian Plate and its hydrocarbon occurrences. GeoArabia (Manama) 6(3):445–504Google Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 2013

Authors and Affiliations

  • Sylvie Leroy
    • 1
  • Philippe Razin
    • 2
  • Julia Autin
    • 1
    • 3
  • François Bache
    • 1
    • 4
  • Elia d’Acremont
    • 1
  • Louise Watremez
    • 1
    • 5
  • Jérémy Robinet
    • 1
    • 2
  • Céline Baurion
    • 1
  • Yoann Denèle
    • 1
    • 6
  • Nicolas Bellahsen
    • 1
  • Francis Lucazeau
    • 7
  • Frédérique Rolandone
    • 1
  • Stéphane Rouzo
    • 1
  • Josep Serra Kiel
    • 8
  • Cécile Robin
    • 9
  • François Guillocheau
    • 9
  • Christel Tiberi
    • 10
  • Clémence Basuyau
    • 7
  • Marie-Odile Beslier
    • 11
  • Cynthia Ebinger
    • 12
  • Graham Stuart
    • 13
  • Abdulhakim Ahmed
    • 1
    • 14
  • Khaled Khanbari
    • 15
  • Ismael Al- Ganad
    • 16
  • Philippe de Clarens
    • 17
  • Patrick Unternehr
    • 17
  • Khalfan Al- Toubi
    • 18
  • Ali Al- Lazki
    • 19
  1. 1.ISTePParis Cedex 05France
  2. 2.EGIDBordeauxFrance
  3. 3.GFZ German Research Centre for GeosciencesPostdamGermany
  4. 4.GNS ScienceLower huttNew Zealand
  5. 5.Dalhousie UniverstyHalifaxCanada
  6. 6.GETUniversity ToulouseToulouseFrance
  7. 7.IPG ParisParisFrance
  8. 8.University BarcelonaBarcelonaSpain
  9. 9.Geosciences RennesRennesFrance
  10. 10.Geosciences MontpellierMontpellier cedex 5 France
  11. 11.GéoAzurVillefranche Sur MerFrance
  12. 12.University of RochesterRochesterUSA
  13. 13.University of LeedsLeedsUK
  14. 14.NSOCDhamarYemen
  15. 15.YRSC and University of Sana’aSana’aYemen
  16. 16.GSMRB Sana’aSana’aYemen
  17. 17.Total La DéfenseParis la Defense CedexFrance
  18. 18.EMCUniversity of Sultan QaboosMuskatOman
  19. 19.College of ScienceUniversity of Sultan QaboosMuskatOman

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