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Data
263 datasets found! (Query time: 5 ms)
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März, C; Schnetger, B; Brumsack, H-J (2010): (Table S1) Enrichment factors of all element/Al ratios compared to average shale of IODP Exp302 holes
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März, C; Schnetger, B; Brumsack, H-J (2010): Paleoenvironmental implications of Cenozoic sediments from the central Arctic Ocean (IODP Expedition 302) using inorganic geochemistry. Paleoceanography |
| Size: |
30829 data points |
https://doi.org/10.1594/PANGAEA.831370 - Score: 14.859
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Waddell, LM; Moore, TC (2008): (Table 3) Stable isotope data from the analysis of fish bones and the calculated salinity range in IODP Exp302
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Waddell, LM; Moore, TC (2008): Salinity of the Eocene Arctic Ocean from oxygen isotope analysis of fish bone carbonate. Paleoceanography |
| Size: |
379 data points |
https://doi.org/10.1594/PANGAEA.733925 - Score: 14.859
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Darby, DA (2009): (Table 1) Ice drift distances and times based on a reconstruction of the Arctic Ocean at 15 Ma and today (Exp302, ACEX)
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Darby, DA (2008): Arctic perennial ice cover over the last 14 million years. Paleoceanography |
| Size: |
134 data points |
https://doi.org/10.1594/PANGAEA.711528 - Score: 14.859
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Spofforth, DJA; Pälike, H; Green, DRH (2008): Chemical composition of Eocene sediments of Hole 302-M0004A
https://doi.org/10.1594/PANGAEA.659167 - Score: 14.859
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Krylov, AA; Andreeva, IA; Vogt, C et al. (2008): (Table 1) Relative abundance of terrigenous minerals of Hole 302-M0002A
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Krylov, AA; Andreeva, IA; Vogt, C et al. (2008): A shift in heavy and clay mineral provenance indicates a middle Miocene onset of a perennial sea ice cover in the Arctic Ocean. Paleoceanography |
| Size: |
265 data points |
https://doi.org/10.1594/PANGAEA.707421 - Score: 14.859
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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
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O'Regan, M; Moran, K; Baxter, CDP et al. (2010): Towards ground truthing exploration in the central Arctic Ocean: a Cenozoic compaction history from the Lomonosov Ridge. Basin Research |
| Size: |
24 data points |
https://doi.org/10.1594/PANGAEA.788556 - Score: 14.859
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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
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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: |
252 data points |
https://doi.org/10.1594/PANGAEA.707032 - Score: 14.859
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Spofforth, DJA; Pälike, H; Green, DRH (2008): Element concentration of sediments of Hole 302-M0004A
https://doi.org/10.1594/PANGAEA.659169 - Score: 14.859
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O'Regan, M; King, JW; Backman, J et al. (2008): (Table S3) Possible ties beyond 1215 ka in the faster sedimentation rate age model of IODP Exp302 composite core
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O'Regan, M; King, JW; Backman, J et al. (2008): Constraints on the Pleistocene chronology of sediments from the Lomonosov Ridge. Paleoceanography |
| Size: |
12 data points |
https://doi.org/10.1594/PANGAEA.832426 - Score: 14.859
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März, C; Vogt, C; Schnetger, B et al. (2011): Inorganic geochemistry of IODP Hole 302-M0002A
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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: |
5372 data points |
https://doi.org/10.1594/PANGAEA.786426 - Score: 14.859
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