Data

 

96 datasets found! (Query time: 1 ms)

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71. O'Regan, M; Sakamoto, T; King, JW (2008): (Table 1) Core recovery summary and vertical core offsets (affine) for the meters composite depth and revised meters composite depth scales of Hole 302-M0004A

    Size:

    252 data points

    https://doi.org/10.1594/PANGAEA.707032 - Score: 7.815
72. O'Regan, M; Moran, K; Baxter, CDP et al. (2012): (Table 2) Average elastic properties of sedimentary subunits where consolidation samples were taken from different Holes of IODP Expedition 302

    Size:

    24 data points

    https://doi.org/10.1594/PANGAEA.788556 - Score: 7.815
73. O'Regan, M; Sakamoto, T; King, JW (2008): (Table 3) Tie points of Hole 302-M0004A

    Size:

    33 data points

    https://doi.org/10.1594/PANGAEA.707037 - Score: 7.752
74. Backman, J; Jakobsson, M; Frank, M et al. (2008): (Table 1) Age-Depth control points and sedimentation rates of IODP Exp302 sediments

    Size:

    38 data points

    https://doi.org/10.1594/PANGAEA.705517 - Score: 7.752
75. O'Regan, M; King, JW; Backman, J et al. (2010): (Table 1) Age markers and errors for the last 1215 ka in IODP Exp302

    Abstract:

    Despite its importance in the global climate system, age-calibrated marine geologic records reflecting the evolution of glacial cycles through the Pleistocene are largely absent from the central Arctic Ocean. This is especially true for sediments older than 200 ka. Three sites cored during the Integrated Ocean Drilling Program's Expedition 302, the Arctic Coring Expedition (ACEX), provide a 27 m continuous sedimentary section from the Lomonosov Ridge in the central Arctic Ocean. Two key biostratigraphic datums and constraints from the magnetic inclination data are used to anchor the chronology of these sediments back to the base of the Cobb Mountain subchron (1215 ka). Beyond 1215 ka, two best fitting geomagnetic models are used to investigate the nature of cyclostratigraphic change. Within this chronology we show that bulk and mineral magnetic properties of the sediments vary on predicted Milankovitch frequencies. […]

    Size:

    124 data points

    https://doi.org/10.1594/PANGAEA.733880 - Score: 7.752
76. Haley, BA; Frank, M; Spielhagen, RF et al. (2008): (Table 2) Arctic Ocean down core leachate and bulk digest radiogenic isotope data of IODP Exp302 composite site

    Size:

    413 data points

    https://doi.org/10.1594/PANGAEA.736515 - Score: 7.752
77. O'Regan, M; Sakamoto, T; King, JW (2008): (Table 1) Core recovery summary and vertical core offsets (affine) for the meters composite depth and revised meters composite depth scales of Hole 302-M0004C

    Size:

    54 data points

    https://doi.org/10.1594/PANGAEA.707033 - Score: 7.752
78. O'Regan, M; Sakamoto, T; King, JW (2008): (Table 2) Revised splice tie table for Holes 302-M0002A, 302-M0003A, 302-M0004A and 302-M0004C

    Size:

    524 data points

    https://doi.org/10.1594/PANGAEA.707034 - Score: 7.752
79. O'Regan, M; Moran, K; Baxter, CDP et al. (2012): (Table 3) Statistics summarizing of grain size measurements at consolidation sample from different Holes of IODP Expedition 302

    Size:

    56 data points

    https://doi.org/10.1594/PANGAEA.788557 - Score: 7.752
80. Vogt, C (2008): Relative mineral abundances from bulk fraction X-ray diffraction data of Hole 302-M0002A

    Size:

    21311 data points

    https://doi.org/10.1594/PANGAEA.704929 - Score: 7.752

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