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Harrison, William E; Curiale, Joseph A (1982): (Table 1) Carbon, hydrocarbons and observations at DSDP Holes 67-497 and 67-498A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.817498, Supplement to: Harrison, WE; Curiale, JA (1982): Gas hydrates in sediments of Holes 497 and 498A, Deep Sea Drilling Project Leg 67. In: Abouin, J; von Huene, R; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 67, 591-594, https://doi.org/10.2973/dsdp.proc.67.126.1982

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Abstract:
Gas hydrates are icelike materials that form when specific conditions of temperature, pressure, and gas composition are simultaneously satisfied. Among the first descriptions of gas hydrates under natural conditions was that of Hammerschmidt (1940), who found them in pipelines used to transport natural gas. Milton (1976) indicates that conditions are suitable for the presence of gas hydrates in areas affected by permafrost and cites studies suggesting that large quantities of gas exist in hydrate form.
Project(s):
Coverage:
Median Latitude: 12.849250 * Median Longitude: -90.871850 * South-bound Latitude: 12.711300 * West-bound Longitude: -90.915700 * North-bound Latitude: 12.987200 * East-bound Longitude: -90.828000
Date/Time Start: 1979-06-01T00:00:00 * Date/Time End: 1979-06-05T00:00:00
Minimum DEPTH, sediment/rock: 163.75 m * Maximum DEPTH, sediment/rock: 372.75 m
Event(s):
67-497 * Latitude: 12.987200 * Longitude: -90.828000 * Date/Time: 1979-06-01T00:00:00 * Elevation: -2347.0 m * Penetration: 396.5 m * Recovery: 224.4 m * Location: North Pacific/SLOPE * Campaign: Leg67 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 40 cores; 377.5 m cored; 19 m drilled; 59.5 % recovery
67-498A * Latitude: 12.711300 * Longitude: -90.915700 * Date/Time: 1979-06-05T00:00:00 * Elevation: -5478.0 m * Penetration: 321.5 m * Recovery: 44.8 m * Location: North Pacific/TRENCH * Campaign: Leg67 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 15 cores; 137.5 m cored; 5 m drilled; 32.6 % recovery
Comment:
Sediment depth is given in mbsf. Routine shipboard analyses involve the use of two gas chromatographs (GC units). Gas samples are first analyzed by a Carle GC with a thermal conductivity detector, and from this analysis come the CO2 and C1 data. The Carle unit is relatively insensitive and a Hewlett-Packard GC is employed to quantify C2 and heavier hydrocarbons. Analysis via the Hewlett-Packard is a cold-trap technique in which C1 is not determined. For complete details, consult Whelan (1979).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2Sample code/labelSample labelHarrison, William EDSDP/ODP/IODP sample designation# = minimum
3Sample code/label 2Sample label 2Harrison, William EDSDP/ODP/IODP sample designation# = maximum
4Depth, top/minDepth topmHarrison, William E
5Depth, bottom/maxDepth botmHarrison, William E
6DEPTH, sediment/rockDepth sedmGeocode
7ObservationObsHarrison, William E
8Method commentMethod commHarrison, William E
9Carbon dioxideCO2%Harrison, William Esee reference(s)Minimum
10Carbon dioxideCO2%Harrison, William Esee reference(s)Maximum
11C1 hydrocarbonsC1%Harrison, William Esee reference(s)Minimum
12C1 hydrocarbonsC1%Harrison, William Esee reference(s)Maximum
13C2 hydrocarbonsC2mg/kgHarrison, William Esee reference(s)Minimum
14C2 hydrocarbonsC2mg/kgHarrison, William Esee reference(s)Maximum
15C3 hydrocarbonsC3mg/kgHarrison, William Esee reference(s)Minimum
16C3 hydrocarbonsC3mg/kgHarrison, William Esee reference(s)Maximum
Size:
137 data points

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