Stein, Ruediger (2007): Analysis of organic carbon from Hole 302-M0004B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.548676, In supplement 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, 24(2), 67-73, https://doi.org/10.1016/j.marpetgeo.2006.10.002
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Project(s):
Coverage:
Latitude: 87.866960 * Longitude: 136.174580
Date/Time Start: 2004-09-02T00:00:00 * Date/Time End: 2004-09-02T00:00:00
Minimum DEPTH, sediment/rock: 215.26 m * Maximum DEPTH, sediment/rock: 218.68 m
Event(s):
302-M0004B (ACEX-M4B) * Latitude: 87.866960 * Longitude: 136.174580 * Date/Time: 2004-09-02T00:00:00 * Elevation: -1287.9 m * IGSN: IBCR0302RHWS001 * Penetration: 218 m * Recovery: 7.31 m * Location: Arctic Ocean * Campaign: Exp302 (Arctic Coring Expedition, ACEX) * Basis: CCGS Captain Molly Kool (Vidar Viking)
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
171 data points
Data
1 Depth sed [m] | 2 Depth comp [mcd] | 3 Sample label | 4 TOC [%] | 5 S1 HC/sed [mg/g] | 6 S2 HC/sed [mg/g] | 7 S3 CO2/sed [mg/g] | 8 Tmax [°C] | 9 HI, HC/TOC [mg/g] | 10 OI, CO2/TOC [mg/g] |
---|---|---|---|---|---|---|---|---|---|
215.26 | 208.97 | 302-M0004B-3H-1,26 | 1.17 | 0.09 | 0.750 | 1.20 | 389 | 64 | 103 |
215.46 | 209.17 | 302-M0004B-3H-1,46 | 1.38 | 0.10 | 1.390 | 1.10 | 395 | 101 | 80 |
215.66 | 209.37 | 302-M0004B-3H-1,66 | 2.18 | 0.15 | 1.110 | 2.31 | 381 | 51 | 106 |
215.86 | 209.57 | 302-M0004B-3H-1,86 | 1.84 | 0.12 | 1.620 | 1.44 | 396 | 88 | 78 |
216.06 | 209.77 | 302-M0004B-3H-1,106 | 1.14 | 0.09 | 0.780 | 0.97 | 389 | 69 | 85 |
216.26 | 209.97 | 302-M0004B-3H-1,126 | 0.94 | 0.10 | 0.980 | 1.08 | 387 | 104 | 115 |
216.46 | 210.17 | 302-M0004B-3H-1,146 | 1.48 | 0.11 | 0.570 | 1.56 | 374 | 39 | 106 |
216.57 | 210.28 | 302-M0004B-3H-2,6 | 1.45 | 0.12 | 0.580 | 1.65 | 363 | 40 | 114 |
216.77 | 210.48 | 302-M0004B-3H-2,26 | 1.63 | 0.14 | 1.410 | 1.21 | 386 | 86 | 74 |
216.97 | 210.68 | 302-M0004B-3H-2,46 | 2.02 | 0.18 | 1.840 | 1.57 | 394 | 91 | 78 |
217.17 | 210.88 | 302-M0004B-3H-2,66 | 1.80 | 0.15 | 1.630 | 1.27 | 391 | 90 | 70 |
217.37 | 211.08 | 302-M0004B-3H-2,86 | 2.85 | 0.24 | 3.340 | 1.94 | 396 | 117 | 68 |
217.57 | 211.28 | 302-M0004B-3H-2,106 | 2.75 | 0.24 | 3.300 | 2.10 | 399 | 120 | 76 |
217.77 | 211.48 | 302-M0004B-3H-2,126 | 2.41 | 0.22 | 2.270 | 1.89 | 389 | 94 | 79 |
217.97 | 211.68 | 302-M0004B-3H-2,146 | 2.54 | 0.26 | 3.220 | 1.79 | 400 | 127 | 70 |
218.08 | 211.79 | 302-M0004B-3H-3,6 | 2.60 | 0.27 | 3.420 | 1.72 | 408 | 132 | 66 |
218.28 | 211.99 | 302-M0004B-3H-3,26 | 2.40 | 0.21 | 2.790 | 1.61 | 400 | 116 | 67 |
218.48 | 212.19 | 302-M0004B-3H-3,46 | 2.57 | 0.22 | 2.910 | 1.68 | 400 | 113 | 65 |
218.68 | 212.39 | 302-M0004B-3H-3,66 | 2.47 | 0.24 | 1.530 | 2.21 | 382 | 62 | 89 |