Grain size and mineral compositions of Pacific red clays
| Cobertura |
MEDIAN LATITUDE: 18.669277 * MEDIAN LONGITUDE: -174.889227 * SOUTH-BOUND LATITUDE: 17.485000 * WEST-BOUND LONGITUDE: 165.690000 * NORTH-BOUND LATITUDE: 20.171700 * EAST-BOUND LONGITUDE: -141.146700 |
|---|---|
| Data(s) |
13/03/1986
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| Resumo |
Hypotheses of origin of ocean deep red clays are under discussion. On an example of the Pacific Ocean grain size, mineralogy and chemical composition of clays are considered. It is shown that they formed from atmospheric dust and andesite pyroclastics. Accumulation of the clays occurred through deposition particle-by-particle and by pellet transport. |
| Formato |
application/zip, 2 datasets |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.777553 doi:10.1594/PANGAEA.777553 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
Supplement to: Logvinenko, Nikolay V; Orlova, LV (1986): On origin of deep sea red clays. Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 21(1), 12-21 |
| Palavras-Chave | #<1 µm; >10 µm; 10-5 µm; 5-1 µm; Archive of Ocean Data; ARCOD; Chl; Chlorite; Depth; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Depth bot; Depth top; DM9; DM9-611; DM9-612; DM9-613; DM9-619; DM9-643; DM9-645; Dmitry Mendeleev; Event; GC; Grab; GRAB; Grain size analysis after Petelin (1967, Nauka, Moscow); Gravity corer; Hydromica; Kaolinite; Kln; Mixed layer clay minerals; Mix layer; Mnt; Montmorillonite; MULT; Multiple investigations; Northeast Pacific; North Pacific; Northwest Pacific; Size fraction < 0.001 mm, clay; Size fraction > 0.010 mm; Size fraction 0.005-0.001 mm; Size fraction 0.010-0.005 mm; X-ray diffraction (XRD) |
| Tipo |
Dataset |
