(Table 2) Relative contents of clay minerals in aeolian pelagic clays from the Pacific Ocean
Cobertura |
MEDIAN LATITUDE: 26.811340 * MEDIAN LONGITUDE: -168.091680 * SOUTH-BOUND LATITUDE: 19.950000 * WEST-BOUND LONGITUDE: 170.966700 * NORTH-BOUND LATITUDE: 34.996700 * EAST-BOUND LONGITUDE: -144.071700 * MINIMUM DEPTH, sediment/rock: 0.175 m * MAXIMUM DEPTH, sediment/rock: 2.865 m |
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Data(s) |
09/03/1988
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Resumo |
For determining importance, composition, and history of aerosol material accumulation in formation of pelagic clays a study with use of light microscopy and scanning electron microscopy, X-ray diffractometry, and chemical methods has been carried out. |
Formato |
text/tab-separated-values, 128 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.777354 doi:10.1594/PANGAEA.777354 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Fonte |
P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow Supplement to: Kuznetsov, AG (1988): Aeolian type of pelagic clays from the North Pacific. Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 23(3), 122-128 |
Palavras-Chave | #Archive of Ocean Data; ARCOD; Chlorite; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; GC; Gravity corer; Hydromica; Kaolinite; Latitude of event; Longitude of event; Montmorillonite; Sediment type; Sum; VITYAZ; Vityaz (ex-Mars); Vityaz-29; VITYAZ3784-GC; VITYAZ4084-GC; VITYAZ4096-GC; VITYAZ4303-GC; VITYAZ4351-GC; X-ray diffraction (XRD) |
Tipo |
Dataset |