Galimov, Erik M; Kodina, Ludmilla A (1982): (Table 25) Ratios of individual hydrocarbons in gas samples from DSDP Hole 50-416A [dataset]. V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Moscow, PANGAEA, https://doi.org/10.1594/PANGAEA.737430, In supplement to: Galimov, EM; Kodina, LA (1982): Study of Organic Matter and Gases in Sedimentary Strata of the World Ocean. Moscow, Nauka, 228 pp
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Project(s):
Archive of Ocean Data (ARCOD)
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 32.836300 * Longitude: -10.801000
Date/Time Start: 1976-09-29T00:00:00 * Date/Time End: 1976-09-29T00:00:00
Minimum DEPTH, sediment/rock: 454.75 m * Maximum DEPTH, sediment/rock: 1581.50 m
Event(s):
50-416A * Latitude: 32.836300 * Longitude: -10.801000 * Date/Time: 1976-09-29T00:00:00 * Elevation: -4191.0 m * Penetration: 1624 m * Recovery: 295.8 m * Location: North Atlantic * Campaign: Leg50 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 57 cores; 622.1 m cored; 0 m drilled; 47.5 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Galimov, Erik M | DSDP/ODP/IODP sample designation | ||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 3 | Depth, top/min | Depth top | m | Galimov, Erik M | ||
| 4 | Depth, bottom/max | Depth bot | m | Galimov, Erik M | ||
| 5 | Epoch | Epoch | Galimov, Erik M | |||
| 6 | Methane/C2+ hydrocarbons ratio | C1/C2+ | Galimov, Erik M | Calculated | ||
| 7 | Ratio | Ratio | Galimov, Erik M | Calculated | C2/C3 | |
| 8 | Ratio | Ratio | Galimov, Erik M | Calculated | C3/(i-C4 + n-C4) | |
| 9 | Ratio | Ratio | Galimov, Erik M | Calculated | i-C4 / n-C4 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
248 data points
Data
| 1 Sample label (DSDP/ODP/IODP sample designation) | 2 Depth sed [m] | 3 Depth top [m] | 4 Depth bot [m] | 5 Epoch | 6 C1/C2+ (Calculated) | 7 Ratio (C2/C3, Calculated) | 8 Ratio (C3/(i-C4 + n-C4), Calculated) | 9 Ratio (i-C4 / n-C4, Calculated) |
|---|---|---|---|---|---|---|---|---|
| 50-416A-3 | 454.75 | 450.0 | 459.5 | Late Oligocene | 6300 | |||
| 50-416A-5 | 758.75 | 754.0 | 763.5 | Albian - Early Eocene | 3100 | 70.0 | ||
| 50-416A-6 | 891.75 | 887.0 | 896.5 | Early Aptian | 4660 | 93.0 | ||
| 50-416A-7 | 1042.25 | 991.5 | 1093.0 | Hauterivian | 2080 | 4.6 | 1.0 | 1.6 |
| 50-416A-9 | 1181.15 | 1176.9 | 1185.4 | Hauterivian | 700 | |||
| 50-416A-11 | 1199.55 | 1194.8 | 1204.3 | Hauterivian | 120 | |||
| 50-416A-12 | 1209.05 | 1204.3 | 1213.8 | Hauterivian | 122 | 7.4 | 14.0 | 1.5 |
| 50-416A-13 | 1218.10 | 1213.8 | 1222.4 | Hauterivian | 200 | 19.0 | ||
| 50-416A-14 | 1228.15 | 1223.4 | 1232.9 | Valanginian | 151 | 16.6 | ||
| 50-416A-15 | 1237.70 | 1232.9 | 1242.5 | Valanginian | 300 | 45.0 | ||
| 50-416A-16 | 1247.25 | 1242.5 | 1252.0 | Valanginian | 348 | 35.0 | ||
| 50-416A-17 | 1256.75 | 1252.0 | 1261.5 | Valanginian | 160 | 8.3 | ||
| 50-416A-18 | 1266.25 | 1261.5 | 1271.0 | Valanginian | 330 | 8.0 | ||
| 50-416A-19 | 1274.25 | 1271.0 | 1277.5 | Valanginian | 236 | 5.3 | ||
| 50-416A-20 | 1282.25 | 1277.5 | 1287.0 | Valanginian | 263 | 6.4 | 1.8 | 1.2 |
| 50-416A-21 | 1294.75 | 1290.0 | 1299.5 | Valanginian | 86 | 2.9 | 0.7 | 1.0 |
| 50-416A-22 | 1304.30 | 1299.5 | 1309.1 | Valanginian | 150 | 2.8 | 1.7 | 1.0 |
| 50-416A-23 | 1313.85 | 1309.1 | 1318.6 | Valanginian | 149 | 2.9 | 1.7 | 1.1 |
| 50-416A-24 | 1323.15 | 1318.6 | 1327.7 | Valanginian | 122 | 2.8 | 1.7 | 1.0 |
| 50-416A-25 | 1332.20 | 1327.7 | 1336.7 | Valanginian | 122 | 2.4 | 1.3 | 0.5 |
| 50-416A-26 | 1341.95 | 1337.2 | 1346.7 | Valanginian | 157 | 3.0 | 1.2 | 0.7 |
| 50-416A-28 | 1361.15 | 1356.4 | 1365.9 | Valanginian | 147 | 2.9 | 1.0 | 1.0 |
| 50-416A-29 | 1370.45 | 1365.7 | 1375.2 | Valanginian | 59 | 1.8 | 2.0 | 1.0 |
| 50-416A-30 | 1379.90 | 1375.2 | 1384.6 | Valanginian | 69 | 2.6 | 0.9 | 0.6 |
| 50-416A-31 | 1384.60 | 1384.6 | 1394.1 | Valanginian | 130 | 2.5 | ||
| 50-416A-32 | 1398.85 | 1394.1 | 1403.6 | Valanginian | 81 | 1.9 | 2.4 | 0.3 |
| 50-416A-34 | 1411.60 | 1406.8 | 1416.4 | Valanginian | 120 | 2.0 | 1.5 | 0.8 |
| 50-416A-36 | 1430.20 | 1425.4 | 1435.0 | Valanginian | 160 | 1.8 | ||
| 50-416A-40 | 1459.20 | 1454.5 | 1463.9 | Valanginian | 100 | 2.2 | 1.7 | 0.2 |
| 50-416A-45 | 1505.90 | 1501.2 | 1510.6 | Valanginian | 4 | 1.3 | 2.7 | 0.2 |
| 50-416A-49 | 1543.85 | 1539.1 | 1548.6 | Berriasian | 253 | 1.9 | 0.8 | |
| 50-416A-50 | 1553.30 | 1548.6 | 1558.0 | Berriasian | 195 | 1.9 | 0.9 | 0.5 |
| 50-416A-51 | 1563.00 | 1558.6 | 1567.4 | Berriasian | 248 | 3.1 | 0.8 | 1.3 |
| 50-416A-52 | 1572.10 | 1567.4 | 1576.8 | Berriasian | 240 | 1.6 | 2.0 | 1.3 |
| 50-416A-53 | 1581.50 | 1576.8 | 1586.2 | Tithonian - Berriasian | 133 | 1.5 | 1.4 | 0.6 |