(Table 1) Carbon, hydrocarbons and observations at DSDP Holes 67-497 and 67-498A
Cobertura |
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 |
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Data(s) |
31/07/1982
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Resumo |
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. |
Formato |
text/tab-separated-values, 137 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.817498 doi:10.1594/PANGAEA.817498 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Fonte |
Supplement to: Harrison, William E; Curiale, Joseph A (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, doi:10.2973/dsdp.proc.67.126.1982 |
Palavras-Chave | #67-497; 67-498A; C1 hydrocarbons; C2 hydrocarbons; C3 hydrocarbons; Carbon dioxide; Deep Sea Drilling Project; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Leg67; Method comment; North Pacific/SLOPE; North Pacific/TRENCH; Observation; ODP sample designation; Sample code/label; Sample code/label 2; see reference(s) |
Tipo |
Dataset |