Chambers, R L; Erdman, J G (1982): (Table 5) Projection of the natural thermolytic degradation of the extract fraction (lipid and elemental sulfur) of DSDP Sample 66-487-2-3,120-150 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.817738, In supplement to: Chambers, RL; Erdman, JG (1982): Elemental composition and petroleum-generating potential of the methylene chloride extracts from Leg 66 Samples. In: Watkins, JS; Casey Moore, J; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 66, 581-585, https://doi.org/10.2973/dsdp.proc.66.122.1982
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 15.853500 * Longitude: -99.175300
Date/Time Start: 1979-03-24T00:00:00 * Date/Time End: 1979-03-24T00:00:00
Minimum Elevation: -4764.0 m * Maximum Elevation: -4764.0 m
Event(s):
66-487 * Latitude: 15.853500 * Longitude: -99.175300 * Date/Time: 1979-03-24T00:00:00 * Elevation: -4764.0 m * Penetration: 190.5 m * Recovery: 119.6 m * Location: North Pacific/TRENCH * Campaign: Leg66 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 20 cores; 180.5 m cored; 9.5 m drilled; 66.3 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Chambers, R L | DSDP/ODP/IODP sample designation | ||
| 2 | Comment | Comment | Chambers, R L | |||
| 3 | - | - | Chambers, R L | Petroleum | ||
| 4 | Type | Type | Chambers, R L | Petroleum | ||
| 5 | Hydrogen/Carbon ratio | H/C | Chambers, R L | Kerogen | ||
| 6 | Kerogen | Kerogen | % | Chambers, R L | ||
| 7 | Carbon dioxide | CO2 | % | Chambers, R L | Element analyser CHN, LECO | |
| 8 | Water in rock | H2O | % | Chambers, R L | ||
| 9 | Ammonia | NH3 | % | Chambers, R L | ||
| 10 | Chlorophyll a sulfide | H2S | % | Chambers, R L |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
74 data points
Data
| 1 Sample label | 2 Comment | 3 - | 4 Type | 5 H/C | 6 Kerogen [%] | 7 CO2 [%] | 8 H2O [%] | 9 NH3 [%] | 10 H2S [%] |
|---|---|---|---|---|---|---|---|---|---|
| 66-487-2-3,120-150 | Part A. Upon degradation 100% of the sulfur is converted to hydrogen sulfide | Natural gas - methane | 1.3 | ||||||
| 66-487-2-3,120-150 | Part A. Upon degradation 100% of the sulfur is converted to hydrogen sulfide | 0.8 | Natural gas - methane | 1.0 | 51.9 | 2.6 | 2.1 | 0.5 | 41.9 |
| 66-487-2-3,120-150 | Part A. Upon degradation 100% of the sulfur is converted to hydrogen sulfide | 6.4 | Natural gas - methane | 0.7 | 45.8 | 2.9 | 2.3 | 0.5 | 41.9 |
| 66-487-2-3,120-150 | Part A. Upon degradation 100% of the sulfur is converted to hydrogen sulfide | 11.0 | Natural gas - methane | 0.4 | 40.7 | 3.1 | 2.5 | 0.6 | 41.9 |
| 66-487-2-3,120-150 | Part B. Upon degradation 50% of the sulfur is converted to hydrogen sulfide and 50% enters the kerogen | 1.2 | Natural gas - methane | 1.3 | 72.7 | 2.2 | 1.7 | 0.5 | 21.6 |
| 66-487-2-3,120-150 | Part B. Upon degradation 50% of the sulfur is converted to hydrogen sulfide and 50% enters the kerogen | 6.6 | Natural gas - methane | 1.0 | 64.5 | 2.7 | 2.2 | 0.5 | 23.4 |
| 66-487-2-3,120-150 | Part B. Upon degradation 50% of the sulfur is converted to hydrogen sulfide and 50% enters the kerogen | 11.2 | Natural gas - methane | 0.7 | 58.0 | 3.0 | 2.4 | 0.6 | 24.9 |
| 66-487-2-3,120-150 | Part B. Upon degradation 50% of the sulfur is converted to hydrogen sulfide and 50% enters the kerogen | 15.1 | Natural gas - methane | 0.4 | 52.3 | 3.2 | 2.5 | 0.6 | 26.2 |