Collins, E.S., Kuhnt, W., Scott, D.B. (1996). Tithonian benthic foraminifers from Hole 901A. In Proceedings of the Ocean Drilling Program, Whitmarsh, R.B., Sawyer, D.S., Klaus, A. and Masson, D.G. (eds). Scientific Results, College Station, TX.
Cresswell, D.J.F. (2018). Continental break-up at the Galicia Margin. PhD thesis, University of Birmingham [Online]. Available at: http://etheses.bham.ac.uk/id/eprint/8712.
Davis, M. and Kusznir, N.J. (2004). Depth-dependent lithospheric stretching at rifted continental margins. In Proceedings of NSF Rifted Margins Theoretical Institute, Karner, G.D. (ed.). Columbia University Press, New York.
Davy, R.G., Minshull, T.A., Bayrakci, G., Bull, J.M., Klaeschen, D., Papenberg, C., Reston, T.J., Sawyer, D.S., Zelt, C.A. (2016). Continental hyperextension, mantle exhumation, and thin oceanic crust at the continent–ocean transition, West Iberia: New insights from wide-angle seismic. Journal of Geophysical Research: Solid Earth, 121, 3177–3199.
Davy, R.G., Morgan, J.V., Minshull, T.A., Bayrakci, G., Bull, J.M., Klaeschen, D., Reston, T.J., Sawyer, D.S., Lymer, G., Cresswell, D. (2018). Resolving the fine-scale velocity structure of continental hyperextension at the Depp Galicia Margin using full-waveform inversion. Geophysical Journal International, 212(1), 244–263.
Dean, S.M., Minshull, T.A., Whitmarsh, R.B., Louden, K.E. (2000). Deep structure of the ocean–continent transition in the southern Iberia Abyssal Plain from seismic refraction profiles: The IAM–9 transect at 40°20ʹN. Journal of Geophysical Research, 105(B3), 5859–5885.
Driscoll, N.W. and Karner, G.D. (1998). Lower crustal extension across the Northern Carnarvon basin, Australia: Evidence for an eastward dipping detachment. Journal of Geophysical Research, 103, 4975–4991, doi.org/10.1029/97JB03295.
Druet, M., Muñoz-Martín, A., Granja-Bruña, J.L., Carbó-Gorosabel, A., Acosta, J., Llanes, P., Ercilla, G. (2018). Crustal structure and continent-ocean boundary along the Galicia continental margin (NW Iberia): Insights from combined gravity and seismic interpretation. Tectonics, 37, 1576–1604, doi.org/10.1029/2017TC004903.
Eagles, G., Pérez–Diaz, L., Scarselli, N. (2015). Getting over continent ocean boundaries. Earth–Science Reviews, 1–56, doi.org/10.1016/j.earscirev.2015.10.009.
Funck, T., Hopper, J.R., Larsen, H.C., Louden, K.E., Tucholke, B.E., Holbrook, W.S. (2003). Crustal structure of the ocean–continent transition at Flemish Cap: Seismic refraction results. Journal of Geophysical Research, 108, 2531, doi:10.1029/2003JB002434.
Gillard, M., Autin, J., Manatschal, G., Sauter, D., Munschy, M., Schaming, M. (2015). Tectonomagmatic evolution of the final stages of rifting along the deep conjugate Australian-Antarctic magma-poor rifted margins: Constraints from seismic observations. Tectonics, 34(4), 753–783.
Hoffmann, H.-J. and Reston, T.J. (1992). Nature of the S reflector beneath the Galicia Banks rifted margin: Preliminary results from prestack depth migration. Geology, 20(12), 1091–1094, doi.org/10.1130/0091-7613(1992)020<1091: NOTSRB>2.3.CO;2.
Hopper, J.R., Funck, T., Tucholke, B.E., Larsen, H.C., Holbrook, W.S., Louden, K.E., Shillington, D., Lau, H. (2004). Continental breakup and the onset of ultraslow seafloor spreading off Flemish Cap on the Newfoundland rifted margin. Geology, 32, 93–96.
Huismans, R. and Beaumont, C. (2011). Depth-dependent extension, two-stage breakup and cratonic underplating at rifted margins. Nature, 473(7345), 74–78.
Krawczyk, C.M., Reston, T.J., Beslier, M.-O., Boillot, G. (1996). Evidence for detachment tectonics on the iberia abyssal plain margin. Proc. ODP, Sci. Results, 149, 603–615.
Lau, K.W.H., Louden, K.E., Deemer, S., Hall, J., Hopper, J.R. Tucholke, B.E., Holbrook, W.S., Larsen, H.C. (2006). Crustal structure across the grand banks – Newfoundland basin continental margin. II. Results from a seismic reflection profile. Geophysical Journal International, 167(1), 157–170, doi.org/10.1111/j. 1365-246X.2006.02989.x.
Le Pichon, X. and Barbier, F. (1987). Passive margin formation by low-angle faulting within the upper crust: The northern Bay of Biscay margin. Tectonics, 6, 133–150.
Lymer, G., Cresswell, D., Reston, T.J., Bull, J.M., Sawyer, D.S., Morgan, J.K., Stevenson, C., Causer, A., Minshull, T.A., Shillington, D.S. (2019). The development of detachment faulting and asymmetry during 3D continental breakup. Earth Planetary Science Letters, 515, 90–99.
Malod, J.A. and Mauffret, A. (1990). Iberian plate motions during the Mesozoic. Tectonophysics, 184(3–4), 261–278, doi.org/10.1016/0040-1951(90)90443-C.
Manatschal, G., Froitzheim, N., Rubenach, M., Turrin, B.D. (2001). The role of detachment faulting in the formation of an ocean-continent transition: Insights from the Iberia Abyssal Plain. In Non-Volcanic Rifting of Continental Margins: A Comparison of Evidence from Land and Sea, Wilson R.C.L., Whitmarsh, R.B., Taylor, B., Froitzheim, N. (eds). Geological Society, London.
Manatschal, G., Lavier, L., Chenin, P. (2015). The role of inheritance in structuring hyperextended rift systems: Some considerations based on observations and numerical modeling. Gondwana Research, 27(1), 140–164.
Marrett, R. and Allmendinger, R.W. (1992). Amount of extension on “small’ faults: An example from the Viking graben. Geology, 20(1), 47–50.
Mauffret, A. and Montadert, L. (1987). Rift tectonics on the passive continental margin off Galicia (Spain), Marine and Petroleum Geology, 4(1), 49–70, doi.org/10.1016/0264-8172(87)90021-3.
McDermott, K. and Reston, T. (2015). To see, or not to see? Rifted margin extension. Geology, 43(11), 967–970, doi.org/10.1130/G36982.1.
McKenzie, D.P. (1978). Some remarks on the development of sedimentary basins. Earth and Planetary Science Letters, 40, 20–32.
Miles, P., Bouysse, P., De Souza, K. (2012). Structural Map of the Atlantic Ocean. CCGM-CGMW, Paris.
Mohn, G., Karner, G.D., Manatschal, G., Johnson, C.A. (2015). Structural and stratigraphic evolution of the Iberia–Newfoundland hyper-extended rifted margin: A quantitative modelling approach, Geological Society, London, Special Publications, 413, 53–89, doi.org/10.1144/SP413.9.
Muentener, O. and Manatschal, G. (2006). High degrees of melt extraction recorded by spinel harzburgite of the Newfoundland margin: The role of inheritance and consequences for the evolution of the North Atlantic. Earth and Planetary Science Letters, 252, 437–452.
Murillas, J., Mougenot, D.G., Boillot, G., Comas, M.C., Banda, E., Mauffret, A. (1990). Structure and evolution of the Galicia interior basin (Atlantic western Iberian continental margin). Tectonophysics, 184, 297–319.
Neves, M.C., Terrinha, P., Afilhado, A., Moulin, M., Matias, L., Rosas, F. (2009). Response of a multi-domain continental margin to compression: Study from seismic reflection–refraction and numerical modelling in the Tagus Abyssal Plain. Tectonophysics, 468(1–4), 113–130, doi.org/10.1016/j.tecto.2008.05.008.
Osmundsen, P.T., Peron-Pinvidic, G., Ebbing, J., Erratt, D., Fjellanger, E., Bergslien, D., Syvertsen, S.E. (2016). Extension, hyperextension and mantle exhumation offshore Norway: A discussion based on 6 crustal transects. Norwegian Journal of Geology, 96(4), 343–372.
Pérez-Gussinyé, M. and Reston, T.J. (2001). Rheological evolution during extension at passive non-volcanic margins: Onset of serpentinization and development of detachments to continental break-up. Journal of Geophysical Research, 106, 3691–3975.
Pérez-Gussinyé, M., Ranero, C.R., Reston, T.J., Sawyer, D. (2003).