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Maud Rise

Holland D.M. (2001). Explaining the Weddell Polynya A large ocean eddy shed at Maud Rise. Science, 292, 1697-1700. [Pg.530]

Eocene to Oligocene Hole 689B, Maud Rise, Antarctica. Paleoceanography 10(2), 327-346. [Pg.3423]

ODP Site 689 was cored on the eastern flank of Maud Rise in the Weddell Sea (Barker et al. 1988). Hole 689B (64°31.009 S 03°05.996 E) was drilled to 297.3 m. Age control is from foraminifera, nannofossils, diatoms and palaeomagnetics. The Eocene extends from about 130 to 200 mbsf, with a sediment accumulation rate of 4-4.5 m/m.yr. The sediment is described as nannofossil ooze and chalk deposited in a pelagic environment (Barker et al. 1988). [Pg.62]

Fig. 1. Comparison of four specimens of Subbotina limperta from four localities, ODP Site 689 - Maud Rise (a, e, i, m, q, u), ODP Site 1135 - Kergeulen Plateau (b, f, j, n, r, v), Hampden Beach (c, g, k, o, s, w), ODP Site 647 - North Atlantic (d, h, 1, p, t, x). RLM photos taken with the specimens submerged in water (a-d) are compared to SEM photographs of the same specimens (e—x). Scale bar is 200 jam for (a—h). Scale bars are 10 (am in (i—1) and 2 (am in (m-x). Fig. 1. Comparison of four specimens of Subbotina limperta from four localities, ODP Site 689 - Maud Rise (a, e, i, m, q, u), ODP Site 1135 - Kergeulen Plateau (b, f, j, n, r, v), Hampden Beach (c, g, k, o, s, w), ODP Site 647 - North Atlantic (d, h, 1, p, t, x). RLM photos taken with the specimens submerged in water (a-d) are compared to SEM photographs of the same specimens (e—x). Scale bar is 200 jam for (a—h). Scale bars are 10 (am in (i—1) and 2 (am in (m-x).
O Connell S.B., 1990. Variations in upper cretaceous and Cenozoic calcium carbonate percentages, Maud Rise, Weddell Sea, Antarctica. In Barker RE, Kennett J.R et al. (eds) Proceedings of the Ocean Drilling Program, Scientific Results 113, College Station, TX (Ocean Program), pp 971-984... [Pg.70]

Magellan Seamount 406 Manihiki Plateau 393 Manus Basin 459,470 Mariana Trough 470 Marianas back-arc 459,471 Maud Rise 40... [Pg.574]

Fig. 14.2 Queen (or Dronning) Maud Land contains groups of nunataks composed of the Jurassic Kirwan Volcanics. The groups of nunataks are identified by number 1, Vestfjella 2, Fossilryggen 3, Mannefallknausane 4, Heimefrontfjella 5, Bjornnutane 6, Sembberget and 7, Kirwan Escarpment. These groups of nunataks rise above the surface of the East Antarctic ice sheet which covers the entire area on this map (Adapted from Fig. 1 of Fumes et al. (1987))... Fig. 14.2 Queen (or Dronning) Maud Land contains groups of nunataks composed of the Jurassic Kirwan Volcanics. The groups of nunataks are identified by number 1, Vestfjella 2, Fossilryggen 3, Mannefallknausane 4, Heimefrontfjella 5, Bjornnutane 6, Sembberget and 7, Kirwan Escarpment. These groups of nunataks rise above the surface of the East Antarctic ice sheet which covers the entire area on this map (Adapted from Fig. 1 of Fumes et al. (1987))...
Bell, F.G. and Maud, R.R. 1995. Expansive clays and construction, especially of low-rise strucfures a viewpoint from Natal, South Africa. Environmental and Engineering Geoscience, 1, 41-59. [Pg.562]

See other pages where Maud Rise is mentioned: [Pg.1796]    [Pg.282]    [Pg.59]    [Pg.59]    [Pg.69]    [Pg.69]    [Pg.38]    [Pg.40]    [Pg.42]    [Pg.1796]    [Pg.282]    [Pg.59]    [Pg.59]    [Pg.69]    [Pg.69]    [Pg.38]    [Pg.40]    [Pg.42]    [Pg.486]    [Pg.219]    [Pg.266]   
See also in sourсe #XX -- [ Pg.282 ]

See also in sourсe #XX -- [ Pg.59 , Pg.69 ]



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