(Table 1) Chemistry of two samples of the red weathered layer at DSDP Hole 55-432A
| Cobertura |
LATITUDE: 41.333800 * LONGITUDE: 170.379000 * DATE/TIME START: 1977-08-06T00:00:00 * DATE/TIME END: 1977-08-06T00:00:00 * MINIMUM ELEVATION: -1310.0 m * MAXIMUM ELEVATION: -1310.0 m |
|---|---|
| Data(s) |
28/11/1980
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| Resumo |
One argument for the subaerial formation of Nintoku Seamount in the Emperor chain is the occurrence of a red claystone interlayered between two basalt flows in Hole 432A. Detailed study of this material, presented here, defines its nature and composition and strongly indicates its subaerial formation. |
| Formato |
text/tab-separated-values, 56 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.823433 doi:10.1594/PANGAEA.823433 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
Supplement to: Karpoff, Anne Marie (1980): The claystone layer between two basalt flows in Hole 432A: An argument for the emergence of Nintoku Seamount. In: Jackson, ED; Koisumi, I; et al., (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 55, 707-711, doi:10.2973/dsdp.proc.55.132.1980 |
| Palavras-Chave | #55-432A; Aluminium oxide; Barium; Boron; Calcium oxide; Chromium; Cobalt; Copper; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Gallium; Glomar Challenger; Iron/Titanium ratio; Iron oxide, Fe2O3; Lead; Leg55; Loss on ignition; Magnesium oxide; Manganese/Iron ratio; Manganous manganic oxide; Nickel; North Pacific/TERRACE; ODP sample designation; Potassium oxide; Ratio; Sample code/label; see reference(s); Silicon/Aluminium ratio; Silicon dioxide; Sodium oxide; Strontium; Titanium oxide; Total; Vanadium; Zinc |
| Tipo |
Dataset |
