Herbin, Jean-Paul; Deroo, Gerard; Roucaché, J (1983): (Table 2) Carbonate, organic carbon, and pyrolysis at DSDP Hole 44-391C [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.809910, In supplement to: Herbin, J-P et al. (1983): Organic geochemistry in the Mesozoic and Cenozoic formations of Site 534, Leg 76, Blake-Bahama Basin, and comparison with Site 391, Leg 44. In: Sheridan, RE; Gradstein, FM; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 76, 481-493, https://doi.org/10.2973/dsdp.proc.76.117.1983
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 28.226800 * Longitude: -75.616700
Date/Time Start: 1975-09-02T00:00:00 * Date/Time End: 1975-09-02T00:00:00
Minimum DEPTH, sediment/rock: 668.98 m * Maximum DEPTH, sediment/rock: 1393.51 m
Event(s):
44-391C * Latitude: 28.226800 * Longitude: -75.616700 * Date/Time: 1975-09-02T00:00:00 * Elevation: -4974.0 m * Penetration: 1412 m * Recovery: 213.7 m * Location: North Atlantic/BASIN * Campaign: Leg44 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 50 cores; 469.5 m cored; 22 m drilled; 45.5 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Sample code/label | Sample label | Herbin, Jean-Paul | DSDP/ODP/IODP sample designation | ||
2 | DEPTH, sediment/rock | Depth sed | m | Geocode – mbsf | ||
3 | Formation | Formation | Herbin, Jean-Paul | |||
4 | Lithologic unit/sequence | Unit | Herbin, Jean-Paul | |||
5 | Carbon, pyrolysis mineral | pyroMinC | % | Herbin, Jean-Paul | Element analyser CHN, LECO | |
6 | Calcium carbonate | CaCO3 | % | Herbin, Jean-Paul | Equivalent | |
7 | Carbon, organic, total | TOC | % | Herbin, Jean-Paul | Element analyser CHN, LECO | |
8 | Hydrogen index, mass HC, per unit mass total organic carbon | HI, HC/TOC | mg/g | Herbin, Jean-Paul | Rock eval pyrolysis (Espitalié et al. 1977) | |
9 | Oxygen index, mass CO2, per unit mass total organic carbon | OI, CO2/TOC | mg/g | Herbin, Jean-Paul | Rock eval pyrolysis (Espitalié et al. 1977) | |
10 | Petroleum potential | PP | mg HC/g | Herbin, Jean-Paul | Rock eval pyrolysis (Espitalié et al. 1977) | |
11 | Pyrolysis temperature maximum | Tmax | °C | Herbin, Jean-Paul | Rock eval pyrolysis (Espitalié et al. 1977) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
886 data points
Data
1 Sample label | 2 Depth sed [m] | 3 Formation | 4 Unit | 5 pyroMinC [%] | 6 CaCO3 [%] | 7 TOC [%] | 8 HI, HC/TOC [mg/g] | 9 OI, CO2/TOC [mg/g] | 10 PP [mg HC/g] | 11 Tmax [°C] |
---|---|---|---|---|---|---|---|---|---|---|
44-391C-4-1,98 | 668.98 | Hatteras Formations | 0.0 | 0 | 0.4 | 159 | 187 | 0.64 | 423 | |
44-391C-4-1,127 | 669.27 | Hatteras Formations | 0.5 | 4 | 0.2 | 39 | 218 | 0.21 | ||
44-391C-5-1,62 | 678.12 | Hatteras Formations | 0.0 | 0 | 0.3 | 167 | 245 | 0.58 | 419 | |
44-391C-6-2,21 | 688.71 | Hatteras Formations | 0.4 | 3 | 0.2 | 0 | 157 | 0.09 | ||
44-391C-6-2,51 | 689.01 | Hatteras Formations | 0.2 | 2 | 0.8 | 3 | 76 | 0.06 | 427 | |
44-391C-6-2,75 | 689.25 | Hatteras Formations | 0.4 | 3 | 0.3 | 6 | 156 | 0.14 | 399 | |
44-391C-6-2,102 | 689.52 | Hatteras Formations | 0.8 | 6 | 0.9 | 0 | 83 | 0.08 | ||
44-391C-6-2,139 | 689.89 | Hatteras Formations | 0.8 | 6 | 0.4 | 0 | 126 | 0.07 | ||
44-391C-6-3,102 | 691.02 | Hatteras Formations | 0.3 | 3 | 0.2 | 7 | 271 | 0.06 | ||
44-391C-6-3,145 | 691.45 | Hatteras Formations | 3b | 1.0 | 8 | 0.7 | 39 | 80 | 0.29 | 430 |
44-391C-6-4,12 | 691.62 | Hatteras Formations | 3b | 0.7 | 6 | 0.3 | 21 | 260 | 0.11 | |
44-391C-6-4,118 | 692.68 | Hatteras Formations | 3b | 0.7 | 6 | 1.1 | 13 | 107 | 0.22 | |
44-391C-6-5,82 | 693.82 | Hatteras Formations | 3b | 0.0 | 0 | 1.5 | 50 | 77 | 0.79 | 421 |
44-391C-6-6,84 | 695.34 | Hatteras Formations | 3b | 0.7 | 6 | 0.5 | 0 | 175 | 0.03 | |
44-391C-6-6,144 | 695.94 | Hatteras Formations | 3b | 1.1 | 9 | 0.8 | 7 | 118 | 0.09 | |
44-391C-7-2,18 | 726.68 | Hatteras Formations | 3b | 1.2 | 10 | 1.1 | 15 | 123 | 0.22 | 375 |
44-391C-7-2,86 | 727.36 | Hatteras Formations | 3b | 1.1 | 9 | 1.3 | 23 | 114 | 0.34 | 415 |
44-391C-7-2,101 | 727.51 | Hatteras Formations | 3b | 0.0 | 0 | 1.0 | 27 | 94 | 0.30 | 433 |
44-391C-7-2,135 | 727.86 | Hatteras Formations | 3b | 0.3 | 3 | 1.3 | 21 | 84 | 0.33 | 430 |
44-391C-8-1,95 | 782.96 | Hatteras Formations | 3b | 1.2 | 10 | 1.5 | 39 | 114 | 0.80 | 407 |
44-391C-8-2,33 | 783.83 | Hatteras Formations | 3b | 0.7 | 6 | 1.2 | 13 | 83 | 0.20 | 406 |
44-391C-8-2,59 | 784.09 | Hatteras Formations | 3b | 0.0 | 0 | 3.0 | 77 | 31 | 2.32 | 417 |
44-391C-8-2,145 | 784.95 | Hatteras Formations | 3b | 0.3 | 3 | 1.1 | 17 | 93 | 0.26 | 430 |
44-391C-9-1,71 | 830.21 | Hatteras Formations | 3b | 0.0 | 0 | 1.5 | 66 | 34 | 1.01 | 417 |
44-391C-9-1,88 | 830.38 | Hatteras Formations | 3b | 0.6 | 5 | 0.4 | 0 | 128 | 0.06 | |
44-391C-9-2,10 | 831.10 | Hatteras Formations | 3b | 6.7 | 56 | 0.4 | 38 | 521 | 0.18 | |
44-391C-9-2,56 | 831.56 | Hatteras Formations | 3b | 0.6 | 5 | 0.6 | 19 | 134 | 0.31 | |
44-391C-9-2,86 | 831.86 | Hatteras Formations | 3b | 0.8 | 6 | 0.4 | 19 | 117 | 0.13 | 416 |
44-391C-9-2,108 | 832.08 | Hatteras Formations | 3b | 0.6 | 5 | 2.4 | 88 | 63 | 2.17 | 429 |
44-391C-9-2,126 | 832.26 | Hatteras Formations | 3b | 0.8 | 6 | 0.3 | 24 | 185 | 0.30 | 433 |
44-391C-9-3,145 | 833.95 | Hatteras Formations | 3b | 0.8 | 7 | 1.6 | 43 | 85 | 0.70 | 430 |
44-391C-10-1,101 | 897.61 | Hatteras Formations | 3b | 0.9 | 8 | 1.1 | 14 | 83 | 0.19 | 407 |
44-391C-10-1,131 | 897.81 | Hatteras Formations | 3b | 2.0 | 17 | 0.3 | 0 | 565 | 0.04 | |
44-391C-10-2,67 | 898.67 | Hatteras Formations | 3b | 9.6 | 80 | 0.1 | 62 | 564 | 0.09 | |
44-391C-10-3,42 | 899.92 | Hatteras Formations | 3b | 0.8 | 7 | 0.2 | 44 | 482 | 0.13 | 358 |
44-391C-10-3,127 | 900.27 | Hatteras Formations | 3b | 0.3 | 3 | 0.6 | 13 | 61 | 0.09 | |
44-391C-10-3,145 | 900.45 | Blake-Bahama Formations | 3c | 3.9 | 32 | 2.7 | 88 | 122 | 2.45 | 430 |
44-391C-11-1,10 | 924.60 | Blake-Bahama Formations | 3c | 3.1 | 26 | 1.5 | 38 | 182 | 0.59 | 434 |
44-391C-11-1,97 | 925.47 | Blake-Bahama Formations | 3c | 3.2 | 27 | 0.5 | 24 | 664 | 0.18 | 421 |
44-391C-11-1,108 | 925.58 | Blake-Bahama Formations | 3c | 8.9 | 74 | 2.2 | 171 | 143 | 3.81 | 426 |
44-391C-11-1,149 | 925.99 | Blake-Bahama Formations | 3c | 0.9 | 8 | 4.1 | 141 | 54 | 5.82 | 426 |
44-391C-11-2,22 | 926.22 | Blake-Bahama Formations | 3c | 5.8 | 48 | 4.2 | 257 | 91 | 10.86 | 428 |
44-391C-11-2,80 | 926.80 | Blake-Bahama Formations | 3c | 3.3 | 27 | 2.3 | 118 | 134 | 2.77 | 431 |
44-391C-11-2,101 | 927.01 | Blake-Bahama Formations | 3c | 5.4 | 45 | 0.9 | 29 | 295 | 0.34 | 417 |
44-391C-11-2,145 | 927.45 | Blake-Bahama Formations | 3c | 8.2 | 69 | 0.9 | 58 | 198 | 0.54 | 430 |
44-391C-11-3,39 | 927.89 | Blake-Bahama Formations | 3c | 3.7 | 31 | 2.3 | 104 | 43 | 2.40 | 423 |
44-391C-12-1,46 | 953.46 | Blake-Bahama Formations | 3c | 3.7 | 31 | 2.0 | 174 | 45 | 3.52 | 421 |
44-391C-12-1,51 | 953.51 | Blake-Bahama Formations | 3c | 3.9 | 33 | 2.8 | 202 | 106 | 5.80 | 426 |
44-391C-12-2,48 | 954.98 | Blake-Bahama Formations | 3c | 7.0 | 58 | 0.9 | 80 | 263 | 0.81 | 421 |
44-391C-12-4,120 | 958.70 | Blake-Bahama Formations | 3c | 1.2 | 10 | 1.8 | 53 | 98 | 1.02 | 434 |
44-391C-14-1,127 | 1001.77 | Blake-Bahama Formations | 4a | 3.6 | 30 | 0.4 | 0 | 357 | 0.03 | |
44-391C-14-2,137 | 1003.37 | Blake-Bahama Formations | 4a | 10.8 | 90 | 0.4 | 38 | 183 | 0.17 | 422 |
44-391C-14-3,54 | 1004.04 | Blake-Bahama Formations | 4a | 5.2 | 43 | 1.6 | 63 | 56 | 1.01 | 426 |
44-391C-15-1,114 | 1011.14 | Blake-Bahama Formations | 4a | 2.9 | 24 | 1.1 | 26 | 82 | 0.30 | 423 |
44-391C-15-1,145 | 1011.45 | Blake-Bahama Formations | 4a | 6.5 | 54 | 0.6 | 55 | 334 | 0.39 | |
44-391C-15-3,89 | 1013.69 | Blake-Bahama Formations | 4a | 5.3 | 44 | 0.7 | 23 | 309 | 0.20 | |
44-391C-16-1,7 | 1019.57 | Blake-Bahama Formations | 4a | 2.6 | 22 | 2.0 | 22 | 86 | 0.49 | 427 |
44-391C-16-2,87 | 1021.87 | Blake-Bahama Formations | 4a | 8.3 | 69 | 0.8 | 63 | 248 | 0.52 | 432 |
44-391C-16-3,84 | 1023.34 | Blake-Bahama Formations | 4a | 4.1 | 34 | 0.5 | 0 | 460 | 0.02 | |
44-391C-16-4,16 | 1024.16 | Blake-Bahama Formations | 4a | 10.2 | 85 | 0.4 | 75 | 341 | 0.30 | 430 |
44-391C-16-4,115 | 1025.15 | Blake-Bahama Formations | 4a | 3.2 | 27 | 0.4 | 16 | 386 | 0.07 | |
44-391C-17-2,32 | 1030.82 | Blake-Bahama Formations | 4a | 2.8 | 23 | 0.7 | 27 | 289 | 0.20 | 425 |
44-391C-18-1,132 | 1039.82 | Blake-Bahama Formations | 4a | 3.9 | 33 | 0.8 | 45 | 232 | 0.37 | 428 |
44-391C-20-1,124 | 1058.74 | Blake-Bahama Formations | 4a | 6.1 | 51 | 0.2 | 2 | 344 | 0.01 | |
44-391C-21-4,114 | 1091.64 | Blake-Bahama Formations | 4a | 4.5 | 38 | 0.5 | 11 | 349 | 0.08 | 431 |
44-391C-24-6,46 | 1131.96 | Blake-Bahama Formations | 4b | 4.5 | 38 | 0.8 | 40 | 206 | 0.35 | 410 |
44-391C-25-2,107 | 1136.07 | Blake-Bahama Formations | 4b | 2.5 | 21 | 1.2 | 23 | 154 | 0.29 | 426 |
44-391C-26-3,72 | 1146.72 | Blake-Bahama Formations | 4b | 4.6 | 39 | 1.1 | 70 | 119 | 0.74 | 424 |
44-391C-27-4,58 | 1157.58 | Blake-Bahama Formations | 4b | 4.2 | 35 | 1.3 | 65 | 73 | 0.88 | 429 |
44-391C-28-2,89 | 1164.39 | Blake-Bahama Formations | 4b | 7.0 | 58 | 2.6 | 288 | 45 | 7.54 | 429 |
44-391C-30-3,55 | 1184.55 | Blake-Bahama Formations | 4b | 1.6 | 13 | 1.3 | 56 | 96 | 0.78 | 414 |
44-391C-31-3,80 | 1194.30 | Blake-Bahama Formations | 4b | 3.0 | 25 | 0.8 | 53 | 99 | 0.46 | 425 |
44-391C-32-3,101 | 1204.01 | Blake-Bahama Formations | 4b | 7.4 | 62 | 1.2 | 160 | 53 | 1.92 | 432 |
44-391C-33-2,39 | 1211.39 | Blake-Bahama Formations | 4b | 7.8 | 65 | 0.9 | 154 | 136 | 1.34 | 430 |
44-391C-34-3,69 | 1222.59 | Blake-Bahama Formations | 4c | 8.5 | 71 | 0.2 | 23 | 419 | 0.05 | 430 |
44-391C-35-3,82 | 1232.32 | Blake-Bahama Formations | 4c | 9.8 | 81 | 0.4 | 74 | 222 | 0.27 | 426 |
44-391C-36-3,136 | 1242.36 | Blake-Bahama Formations | 4c | 7.0 | 58 | 0.6 | 54 | 102 | 0.34 | 422 |
44-391C-38-3,40 | 1260.40 | Blake-Bahama Formations | 4d | 5.9 | 49 | 0.4 | 21 | 236 | 0.09 | 423 |
44-391C-39-2,17 | 1268.17 | Blake-Bahama Formations | 4d | 5.6 | 47 | 0.6 | 33 | 146 | 0.20 | 421 |
44-391C-40-3,35 | 1279.35 | Blake-Bahama Formations | 4d | 6.4 | 53 | 0.3 | 37 | 404 | 0.13 | 438 |
44-391C-41-2,102 | 1288.02 | Blake-Bahama Formations | 4d | 6.2 | 51 | 0.2 | 38 | 568 | 0.09 | 440 |
44-391C-42-4,126 | 1300.76 | Blake-Bahama Formations | 4d | 5.0 | 42 | 0.2 | 47 | 536 | 0.12 | 436 |
44-391C-43-3,25 | 1307.75 | Blake-Bahama Formations | 4d | 10.3 | 86 | 0.1 | 52 | 608 | 0.08 | 452 |
44-391C-44-5,27 | 1314.87 | Blake-Bahama Formations | 4d | 5.9 | 49 | 0.2 | 33 | 518 | 0.09 | 434 |
44-391C-45-2,99 | 1325.99 | Cat Cap Formations | 5a | 5.2 | 43 | 0.3 | 23 | 363 | 0.08 | 433 |
44-391C-46-1,32 | 1333.32 | Cat Cap Formations | 5a | 5.5 | 46 | 0.3 | 16 | 309 | 0.06 | 438 |
44-391C-47-1,94 | 1343.44 | Cat Cap Formations | 5a | 4.0 | 33 | 0.3 | 15 | 252 | 0.05 | |
44-391C-48-2,89 | 1354.39 | Cat Cap Formations | 5a | 2.5 | 21 | 0.5 | 33 | 159 | 0.17 | 432 |
44-391C-49-2,45 | 1363.45 | Cat Cap Formations | 5a | 1.4 | 12 | 0.8 | 11 | 71 | 0.10 | |
44-391C-50-1,143 | 1372.43 | Cat Cap Formations | 5b | 3.5 | 29 | 0.8 | 12 | 73 | 0.12 | 431 |
44-391C-51-2,89 | 1382.39 | Cat Cap Formations | 5b | 2.6 | 22 | 0.9 | 11 | 211 | 0.14 | |
44-391C-52-3,51 | 1393.51 | Cat Cap Formations | 5b | 5.7 | 47 | 0.3 | 16 | 396 | 0.07 |