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Data

 
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Windrose

96 datasets found! (Query time: 7 ms)

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  1. Vogt, C (2008): Sum peak hight and area intensities of bulk X-ray diffraction data of Hole 302-M0004C
    Related to:  Vogt, C (2009): Data report: semiquantitative determination of detrital input to ACEX sites based on bulk sample X-ray diffraction data. In: Backman, J., Moran, K., McInroy, D.B., Mayer, L.A., and the Expedition 302 Scientists, Proc. IODP: Edinburgh (Integrated Ocean Drilling Program Management International, Inc.)
    Size:  1248 data points
    https://doi.org/10.1594/PANGAEA.704653 - Score: 5.321

  2. März, C; Vogt, C; Schnetger, B et al. (2011): X-ray diffraction analysis of sediments of IODP Hole 302-M0002A
    Related to:  März, C; Vogt, C; Schnetger, B et al. (2011): Variable Eocene-Miocene sedimentation processes and bottom water redox conditions in the Central Arctic Ocean (IODP Expeditrion 302). Earth and Planetary Science Letters
    Size:  13254 data points
    https://doi.org/10.1594/PANGAEA.747735 - Score: 5.321

  3. Onodera, J; Takahashi, K (2012): (Table 2) Mean abundance of ebridian taxa in each ebridian assemblage group from IODP Exp302
    Related to:  Onodera, J; Takahashi, K (2009): Middle Eocene ebridians from the central Arctic Basin. Micropaleontology
    Size:  52 data points
    https://doi.org/10.1594/PANGAEA.787524 - Score: 5.321

  4. Haley, BA; Frank, M; Spielhagen, RF et al. (2008): Neodymium and Strontium chemistry of IODP Exp302-Composite Site
    Related to:  Haley, BA; Frank, M; Spielhagen, RF et al. (2008): Influence of brine formation on Arctic Ocean circulation over the past 15 million years. Nature Geoscience
    Size:  138 data points
    https://doi.org/10.1594/PANGAEA.769603 - Score: 5.321

  5. Vogt, C (2008): Relative mineral abundances from bulk fraction X-ray diffraction data of Hole 302-M0003A
    Related to:  Vogt, C (2009): Data report: semiquantitative determination of detrital input to ACEX sites based on bulk sample X-ray diffraction data. In: Backman, J., Moran, K., McInroy, D.B., Mayer, L.A., and the Expedition 302 Scientists, Proc. IODP: Edinburgh (Integrated Ocean Drilling Program Management International, Inc.)
    Size:  936 data points
    https://doi.org/10.1594/PANGAEA.704657 - Score: 5.321

  6. Stein, R (2007): Analysis of organic carbon from Hole 302-M0004C
    Related to:  Stein, R (2007): Upper Cretaceous/Lower Tertiary black shales near the North Pole: Organic-carbon origin and source-rock potential. Marine and Petroleum Geology
    Size:  740 data points
    https://doi.org/10.1594/PANGAEA.548677 - Score: 5.312

  7. O'Regan, M; Sakamoto, T; King, JW (2008): (Table 3) Tie points of Hole 302-M0004A
    Related to:  O'Regan, M; Sakamoto, T; King, JW (2008): Data report: Regional stratigraphic correlation and a revised composite depth scale for IODP Expedition 302. In: Backman, J., Moran, K., McInroy, D.B., Mayer, L.A., and the Expedition 302 Scientists, Proc. IODP, 302: Edinburgh (Integrated Ocean Drilling Program Management International, Inc.).
    Size:  33 data points
    https://doi.org/10.1594/PANGAEA.707037 - Score: 5.312

  8. Onodera, J; Takahashi, K (2012): (Table 2) The mean abundances of silicoflagellates of each group from IODP Exp302
    Related to:  Onodera, J; Takahashi, K (2009): Taxonomy and biostratigraphy of middle Eocene silicoflagellates in the central Arctic Basin. Micropaleontology
    Size:  170 data points
    https://doi.org/10.1594/PANGAEA.787453 - Score: 5.312

  9. Backman, J; Jakobsson, M; Frank, M et al. (2008): (Table 1) Age estimates of lithostratigraphic units of Hole 302-M0004A
    Related to:  Backman, J; Jakobsson, M; Frank, M et al. (2008): Age model and core-seismic integration for the Cenozoic Arctic Coring Expedition sediments from the Lomonosov Ridge. Paleoceanography
    Size:  4 data points
    https://doi.org/10.1594/PANGAEA.705519 - Score: 5.312

  10. Spofforth, DJA; Pälike, H; Green, DRH (2008): Element concentration of sediments of Hole 302-M0002A
    Size:  1278 data points
    https://doi.org/10.1594/PANGAEA.659168 - Score: 5.312

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