Abstract
The relief and geophysical characteristics of the bottom in the Drake Passage-Scotia Sea belt have been studied and discussed relatively well in many publications. However, the tectonics and geodynamics of this belt lack a universally recognized interpretation. The ocean bottom is usually viewed as a collage of small fragments of the continental bridge and young oceanic plates formed as a result of spreading in the course of large-scale movements of huge lithospheric plates. The authors of this article propose an alternative hypothesis of the origin of the lithospheric belt of the Drake Passage and the Scotia Sea as an area of a large intercontinental bridge that underwent basification and destruction into large fragments under the conditions of moderate extension and short-term local riftogenesis.
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References
P. F. Barker, “The Antarctic Peninsula Region: Tectonic and Sedimentary Environments,” Terra Antarctica 1(2), 259 (1994).
S. Wise, K. Busen, A. M. Gombos, et al., “Paleontologic and Paleoenvironmental Synthesis for the Southwest Atlantic Ocean Basin Based on Jurassic to Holocene Faunas and Floras from the Falkland Plateau,” in Antarctic Geoscience, Ed. by C. Craddock (Univ. of Wisconsin Press, Madison, 1982) pp. 155–163.
G. B. Udintsev, A. F. Beresnev, N. A. Kurentsova, et al., “The Drake Passage and the Scotia Sea As the Oceanic Gateway of West Antarctica,” in The Structure and History of Lithospheric Development (Paulsen, Moscow, 2010) [in Russian].
G. B. Udintsev and H. W. Schenke, Essays on the Geodynamics of West Antarctica (GEOS, Moscow, 2004) [in Russian].
V. D. Solov’ev, V. G. Bakhmutov, I. N. Korchagin, and S. P. Levashov, “Abyssal Heterogeneities of the Bottom Structures of the Central Segment the Shackleton Fracture Zone (Drake Passage) according to Geophysical Research Data,” Ukrainian Antarctic J., No. 9 (2010).
P. F. Barker, “Scotia Sea Regional Tectonic Evolution: Implications for Mantle Flow and Palaeocirculation,” Earth-Science Reviews 55(1, 2), 1 (2001).
R. Livermore, G. Eagles, P. Morris, and A. Maldonado, “Shackleton Fracture Zone: No Barrier to Early Circumpolar Ocean Circulation,” Geol. 32(9), 797 (2004).
F. Herve, H. Miller, and C. Pimpiev, “Patagonia — Antarctica Connections before Gondwana Break-Up,” in Antarctica: Contributions to Global Earth Sciences, Ed. by D. K. Futterer, D. Damaske, G. Kleinschmidt, E. Tessensohn (Springer, Berlin, 2006), pp. 217–228.
W. H. Choe, J. I. Lee, M. J. Lee, et al., “Origin of E-MORB in a Fossil Spreading Center: The Antarctic-Phoenix Ridge, Drake Passage, Antarctica,” Geosci. J. 11(3), 185 (2007).
V. M. Gordin, “The Anomalous Magnetic Field of the World Ocean and the Vine-Matthews Hypothesis,” in V. M. Gordin, Selected Works (IFZ RAN, Moscow, 2007) [in Russian].
N. A. Kurentsova and G. B. Udintsev, “The Main Features of the Structure and Evolution of the Southern Part of the Scotia Sea, West Antarctic,” Tikhookean. Geol. 23(5), 25 (2004).
N. A. Kurentsova, T. N. Frolova, G. B. Udintsev, and I. A. Roshchina, “Rock Material from the Weddell Sea Floor of the South Ocean,” Russ. J. Pacific Geol. 1(5), 435 (2007).
A. D. Saunders, J. Tarney, S. D. Weavr, and P. F. Barker, “Scotia Sea Floor: Geochemistry of Basalts from the Drake Passage and South Sandwich Spreading Centers,” in Antarctic Geoscience (Univ. of Wisconsin Press, Madison, 1982), pp. 213–222.
R. A. Livermore, D. McAdoo, and K. Marks, “Scotia Sea Tectonics from High-Resolution Satellite Gravity,” Earth Planet. Sci. Lett. 123, 797–800 (1994).
E. M. Rudich, Spreading Oceans: Facts and Hypotheses (Nedra, Moscow, 1984) [in Russian].
The Expeditions ANTARKTIS-XXII/4 and ANTARK-TIS-XXII/5 of the R/V Polarstern in 2005, Ed. by H. W. Schenke and W. Zenk (2006).
G. B. Udintsev and H. W. Schenke, “Undersea Geophysical Research Near the Earth’s South Pole,” Her. Russ. Acad. Sci. 76(6), 549 (2006).
Y. Kristoffersen and J. LaBrecque, “On the Tectonic History and Origin of the Northeast Georgia Rise,” in P. F. Ciesielski, Y. Kristoffersen, et al., Proc. Ocean Drilling Progr., Scientific Results (College Station, 1991), Vol. 114, pp. 23–38.
C. A. Raymond, J. L. LaBrecque, and Y. Kristoffersen, “Islas Orcadas Rise and Meteor Rise: the Tectonic and Depositional History of Two Aseismic Plateaus from Sites 702, 703 and 704,” in P. F. Ciesielski, Y. Kristoffersen, et al., Proc. Ocean Drilling Progr., Scientific Results (College Station, 1991), Vol. 114, pp. 5–22.
V. Toker, P. F. Barker, and C. W. Wise, “Middle Eocene Carbonate-Bearing Marine Sediments from Bruce Bank off Northern Antarctic Peninsula,” in Geological Evolution of Antarctica (Cambridge Univ. Press, 1991), pp. 639–644.
D. T. Sandwell and W. H. Smith, “Marine Gravity Anomaly from Geosat and ERS 1 Satellite Altimetry,” J. Geophys. Res. 102, 10039–10054 (1997).
Additional information
Original Russian Text © G.B. Udintsev, N.A. Kurentsova, H.W. Schenke, V.G. Bakhmutov, V.D. Solov’ev, 2012, published in Vestnik Rossiiskoi Akademii Nauk, 2012, Vol. 82, No. 7, pp. 615–623.
RAS Corresponding Member Gleb Borisovich Udintsev works at the Vernadsky Institute of Geochemistry and Analytical Chemistry, RAS. Natal’ya Alekseevna Kurentsova, Dr. Sci. (Geol.-Mineral.), is a senior researcher at the same institute. Prof. Hans Werner Schenke, Dr. Sci. (Geophys.), is an engineer at the Alfred Wegener Institute of Polar and Marine Research (Germany). Vladimir Georgievich Bakhmutov, Dr. Sci. (Geol.-Mineral.), is a department head at the Subbotin Institute of Geophysics, National Academy of Sciences of Ukraine. Valerii Dmitrievich Solov’ev is a senior researcher at the same institute.
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Udintsev, G.B., Kurentsova, N.A., Schenke, H.W. et al. A new approach to the separation of South America from West Antarctica. Her. Russ. Acad. Sci. 82, 281–289 (2012). https://doi.org/10.1134/S1019331612040077
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DOI: https://doi.org/10.1134/S1019331612040077