Название | Continental Rifted Margins 2 |
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Автор произведения | Gwenn Peron-Pinvidic |
Жанр | Физика |
Серия | |
Издательство | Физика |
Год выпуска | 0 |
isbn | 9781119986942 |
Pérez-Gussinyé, M., Phipps Morgan, J., Reston, T.J., Ranero, C.R. (2006). The rift to drift transition at non-volcanic margins: Insights from numerical modelling. Earth and Planetary Science Letters, 244, 458–473.
Peron-Pinvidic, G., Manatschal, G., Osmundsen, P.T. (2013). Structural comparison of archetypal Atlantic rifted margins: A review of observations and concepts. Marine and Petroleum Geology, 43, 21–47, doi.org/10.1016/j.marpetgeo.2013.02.002.
Peron-Pinvidic, G., Manatschal, G., The “IMAGinING RIFTING” Workshop Participants (2019). Rifted margins: State of the art and future challenges. Frontiers in Earth Science, 7, 218–225.
Pickup, S., Whitmarsh, R.B., Fowler, C.M.R., Reston, T.J. (1996). Insight into the nature of the ocean-continent transition off West Iberia from a deep multichannel seismic reflection profile. Geology, 24, 1079–1082, doi.org/10.1130/0091-7613(1996)024<1079: IITNOT>2.3.CO;2.
Prada, M., Watremez, L., O’Reilly, B., Minshull, T.A., Chen, C., Reston, T.J., Shannon, P., Klaeschen, D., Wagner, G., Gaw, V. (2017). Crustal strain-dependent serpentinisation in the Porcupine Basin, offshore Ireland. Earth and Planetary Science Letters, 474, 148–159.
Ranero, C.R. and Pérez-Gussinyé, M. (2010). Sequential faulting explains the asymmetry and extension discrepancy of conjugate margins. Nature, 468, 294–297.
Reid, I.D. (1994). Crustal structure of a nonvolcanic rifted margin east of Newfoundland. Journal of Geophysical Research, 99, 15161–15180.
Reston, T.J. (1993). Evidence for extensional shear zones in the mantle, offshore Britain, and their implications for the extension of the continental lithosphere. Tectonics, 12(2), 492–506.
Reston, T.J. (1996). The S reflector west of Galicia: The seismic signature of a detachment fault. Geophysical Journal International, 127, 230–244.
Reston, T.J. (2005). Polyphase faulting during the development of the west Galicia rifted margin. Earth and Planetary Science Letters, 237(3–4), 561–576.
Reston, T.J. (2009). The structure, evolution and symmetry of the magma-poor rifted margins of the north and central Atlantic: A synthesis. Tectonophysics, 468(1–4), 6–27.
Reston, T.J. (2010). The opening of the central segment of the south Atlantic: Symmetry and the extension discrepancy. Petroleum Geoscience, 16, 199–206.
Reston, T.J. and McDermott, K. (2014). An assessment of the cause of the “Extension Discrepancy” with reference to the west Galicia margin. Basin Research, 26, 135–153.
Reston, T.J. and Morgan, J.P. (2004). Continental geotherm and the evolution of rifted margins. Geology, 32(2), 133–136, doi.org/10.1130/G19999.1.
Reston, T.J. and Pérez-Gussinyé, M. (2007). Lithospheric extension from rifting to continental breakup at magma-poor margins: Rheology, serpentinisation and symmetry. International Journal of Earth Sciences, 96(6), 1033–1046, doi.org/10.1007/s00531-006-0161-z.
Reston, T.J. and Phipps-Morgan, J. (2004). Continental geotherm and the evolution of rifted margins. Geology, 32(2), 133–136, doi.org/10.1130/G19999.1.
Reston, T.J., Pennell, J., Stubenrauch, A., Walker, I., Pérez-Gussinyé, M. (2001). Detachment faulting, mantle serpentinization, and serpentinite- mud volcanism beneath the Porcupine Basin, southwest of Ireland. Geology, 29(7), 587–590.
Reston, T.J., Leythaeuser, T., Booth-Rea, G., Sawyer, D., Klaeschen, D., Long, C. (2007). Movement along a low-angle normal fault: The S reflector west of Spain. Geochemistry, Geophysics, Geosystems, 8, Q06002.
Ros, E., Pérez-Gussinyé, M., Araujo, M., Thoaldo Romeiro, M., Andrés-Martinez, M., Morgan, J.P. (2017). Lower crustal strength controls on melting and serpentinization at magma-poor margins: Potential implication for the South Atlantic. Geochemistry, Geophysics, Geosystems, 18, 4538–4557, doi.org/10.1002/2017GC007212.
Sawyer, D.S., Whitmarsh, R.B., Klaus, A. et al. (1994). Leg 149. Proceedings of the Ocean Drilling Program, Initial Reports [Online]. Available at: http://www-odp.tamu.edu/publications/149_IR/149TOC.HTM.
Schuba, N.C., Gray, G.G., Morgan, J.K., Sawyer, D.S., Shillington, D.J., Reston, T.J., Bull, J.M., Jordan, B.E. (2018). A low-angle detachment fault revealed: Three-dimensional images of the S-reflector fault zone along the Galicia passive margin. Earth and Planetary Science Letters [Online]. Available at: https://doi.org/10.1016/j.epsl.2018.04.012.
Shillington, D.J., Holbrook, W.S., Van Avendonk, H.J.A., Tucholke, B.E., Hopper, J.R., Louden, K.E., Larsen, H.C., Nunes, G.T. (2006). Evidence for asymmetric nonvolcanic rifting and slow incipient oceanic accretion from seismic reflection data on the Newfoundland margin. Journal of Geophysical Research, 111, B09402.
Sibuet, J.-C. (1992). New constraints on the formation of the non-volcanic continental Galicia-Flemish Cap conjugate margins. Journal of the Geological Society, 149, 829–840.
Sibuet, J.–C., Srivastava, S., Manatschal, G. (2007). Exhumed mantle-forming transitional crust in the Newfoundland–Iberia rift and associated magnetic anomalies, Journal of Geophysical Research, 112, B06105.
Srivastava, S.P., Roest, W.R., Kovacs, L.C., Oakey, G., Lévesque, S., Verhoef, J., Macnab, R. (1990). Motion of Iberia since the Late Jurassic: Results from detailed aeromagnetic measurements in the Newfoundland Basin. Tectonophysics, 184(3–4), 229–260, doi.org/10.1016/0040-1951(90)90442-B.
Stica, J.M., Zalán, P.V., Ferrari, A.L. (2014), The evolution of rifting on the volcanic margin of the Pelotas Basin and the contextualization of the Paraná–Etendeka LIP in the separation of Gondwana in the South Atlantic. Marine and Petroleum Geology, 50, 1–21.
Sutra, E. and Manatschal, G. (2012). How does the continental crust thin in a hyper-extended rifted margin? Insights from the Iberia margin. Geology, 40, 139–142.
Sutra, E., Manatschal, G., Mohn, G., Unternehr, P. (2013). Quantification and restoration of extensional deformation along the western Iberia and Newfoundland rifted margins. Geochemistry, Geophysics, Geosystems, 14, 2575–2597, doi.org/10.1002/ggge.20135.
Thinon, I., Fidalgo-González, L., Réhault, J.-P., Olivet, J.-L. (2001). Déformations pyrénéennes dans le golfe de Gascogne, Comptes Rendus de l’Académie des Sciences – Series IIA. Earth and Planetary Science, 332(9), 561–568, doi.org/10.1016/S1251-8050(01)01576-2.
Tucholke, B.E., Sawyer, D.S., Sibuet, J.C. (2007). Breakup of the Newfoundland-Iberia rift. In Imaging, Mapping and Modelling Continental Lithosphere Extension and Breakup, Karner, G.D., Manatschal, G., Pinheiro, L.M. (eds). Geological Society, London.
Tugend, J., Manatschal, G., Kusznir, N.J. (2015). Spatial and temporal evolution of hyperextended rift systems: Implication for the nature, kinematics, and timing of the Iberian-European plate boundary. Geology, 43(1), 15–18, doi.org/10.1130/G36072.1.
Turner, J.P. and Wilson, P.G. (2009). Structure and composition of the ocean–continent transition at an obliquely divergent transform margin, Gulf of Guinea, West Africa. Petroleum Geoscience, 15, 305–311.
Van Avendonk, H.J., Holbrook, W.S., Nunes, G.T., Shillington, D.J., Tucholke, B.E., Louden, K.E., Larsen, H.C., Hopper, J.R. (2006). Seismic velocity structure of the rifted margin of eastern Grand Banks of Newfoundland, Canada. Journal of Geophysical Research, 111(B11404), doi.org/10.1029/2005JB004156.
Vegas, R., Vázquez, J.T., Olaiz, A.J., Medialdea, T. (2016). Tectonic model for the latest Triassic-Early Jurassic extensional event in and around the Iberian Peninsula. Geogaceta, 60, 23–26.
Welford, K., Hall,