(Table 1) Mineral composition of a Fe-Mn crust broken through by a gravity core at Station AK15-1364
| Cobertura |
LATITUDE: 68.843000 * LONGITUDE: -8.990000 * MINIMUM DEPTH, sediment/rock: 0.080 m * MAXIMUM DEPTH, sediment/rock: 0.425 m |
|---|---|
| Data(s) |
20/02/1976
|
| Formato |
text/tab-separated-values, 144 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.776243 doi:10.1594/PANGAEA.776243 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.776252 Emelyanov, Emelyan M; Blazhchishin, AI; Kharin, Gennady S (1976): On the role of endogenic sources in formation of chemical composition of bottom sediments from the North Atlantic. Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 11(5), 3-21 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
P.P. Shirshov Institute of Oceanology, RAS, Atlantic Branch, Kaliningrad |
| Palavras-Chave | #Aggregates; AK15-1364; Akademik Kurchatov; AKU15; Archive of Ocean Data; ARCOD; Carbonate, authigenic; Chlorite; Clayey aggregates; Counting, binocular; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Feldspar; Foraminifera; GC; Gravity corer; Minerals, other; North Atlantic; Quartz; Size fraction; Sulfides |
| Tipo |
Dataset |
