Galimov, Erik M; Kodina, Ludmilla A (1982): (Table 24) Ratios of individual hydrocarbons in gas samples from DSDP Holes 50-415 and 50-415A [dataset]. V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Moscow, PANGAEA, https://doi.org/10.1594/PANGAEA.737428, 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: 31.028700 * Longitude: -11.651800
Date/Time Start: 1976-09-13T00:00:00 * Date/Time End: 1976-09-13T00:00:00
Minimum DEPTH, sediment/rock: 447.50 m * Maximum DEPTH, sediment/rock: 1036.75 m
Event(s):
50-415A * Latitude: 31.028700 * Longitude: -11.651800 * Date/Time: 1976-09-13T00:00:00 * Elevation: -2794.0 m * Penetration: 1079.5 m * Recovery: 29.5 m * Location: North Atlantic/BASIN * Campaign: Leg50 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 14 cores; 1240 m cored; 19 m drilled; 2.4 % 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:
72 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) |
|---|---|---|---|---|---|---|---|---|
| 50-415A-5 | 447.50 | 443.0 | 452.0 | Paleocene | 3284 | |||
| 50-415A-6 | 480.75 | 452.0 | 509.5 | Paleocene | 3686 | |||
| 50-415A-7 | 514.25 | 509.5 | 519.0 | Middle-Late Cretaceous | 1230 | 20.6 | ||
| 50-415A-8 | 552.25 | 519.0 | 585.5 | Middle-Late Cretaceous | 1156 | 10.9 | 2.4 | 1.2 |
| 50-415A-9 | 647.00 | 642.0 | 652.0 | Cenomanian | 980 | 7.7 | 1.7 | 1.7 |
| 50-415A-10 | 713.75 | 709.0 | 718.5 | Cenomanian | 1135 | 7.4 | 2.0 | 2.2 |
| 50-415A-11 | 799.00 | 794.0 | 804.0 | Cenomanian | 519 | 64.0 | 1.4 | 2.7 |
| 50-415A-12 | 884.75 | 880.0 | 889.5 | Cenomanian | 632 | 6.7 | 1.6 | 2.6 |
| 50-415A-13 | 960.75 | 956.0 | 965.5 | Cenomanian | 332 | 6.0 | 1.3 | 2.7 |
| 50-415A-14 | 1036.75 | 1032.0 | 1041.5 | Albian | 402 | 8.6 | 1.5 | 2.9 |