(Table 4) Molecular composition and concentration of hydrocarbons in hydrothermal sulfides from the Rainbow Hydrothermal Field
| Cobertura |
MEDIAN LATITUDE: 36.230070 * MEDIAN LONGITUDE: -33.902678 * SOUTH-BOUND LATITUDE: 36.230000 * WEST-BOUND LONGITUDE: -33.903550 * NORTH-BOUND LATITUDE: 36.230160 * EAST-BOUND LONGITUDE: -33.902000 * MINIMUM ELEVATION: -2350.0 m * MAXIMUM ELEVATION: -2250.0 m |
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| Data(s) |
11/07/2003
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| Formato |
text/tab-separated-values, 112 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.785881 doi:10.1594/PANGAEA.785881 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.785882 Lein, Alla Yu; Peresypkin, Valery I; Simoneit, Bernd R T (2003): Origin of hydrocarbons in hydrothermal sulfide ores in the Mid-Atlantic Ridge. Translated from Litologiya i Poleznye Iskopaemye, 2003, 5, 451-462, Lithology and Mineral Resources, 38(5), 383-393, http://www.springerlink.com/content/m50328087gu21831/ |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Akademik Mstislav Keldysh; AMK42; AMK42-3956-M1; AMK42-3957-M2; AMK42-3959-M1; AMK42-3982-M1-2; Archive of Ocean Data; ARCOD; Calculated; Carbon Preference Index; Chromatographic; Elevation of event; Event label; Gas chromatography - Mass spectrometry (GC-MS); Hydrocarbons; i-C19/C17 ratio; i-C19/i-C20 ratio; i-C20/C18 ratio; Latitude of event; Longitude of event; MIR; MIR-1; MIR-1 deep-sea manned submersible; MIR-2; MIR-2 deep-sea manned submersible; MIR deep-sea manned submersible; n-Alkane, total per unit sediment mass; Rainbow Hydrothermal Field; Sample code/label; Sum(C10-C22)/sum(C23-C35) n-alkanes ratio; Sum even numbered n-alkanes; Sum n-alkanes C10-C14; Sum n-alkanes C10-C17; Sum n-alkanes C10-C22; Sum n-alkanes C18-C22; Sum n-alkanes C20-C24; Sum n-alkanes C23-C35; Sum odd numbered n-alkanes |
| Tipo |
Dataset |
