(Table 3, page 264), Composition of a manganese micronodule found in a fossil red clay bed from Western Timor
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| Sprache: | en |
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1961
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| _version_ | 1867170061065650176 |
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| author | El Wakeel, S K Riley, J P |
| author_facet | El Wakeel, S K Riley, J P |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Chemical analyses are presented for two Cretaceous clays from Noil Tobee, Timor. Mineralogical examination has shown that they consist principally of quartz, feldspar, illite and chlorite, together with minor amounts of montmorillonite. Both chemically and mineralogically the clays are very similar to the recent argillaceous deep-sea sediments of the Pacific and Indian Oceans, which confirms Molengraaff's theory (1921) that they are of deep-sea origin. Further confirmation of this theory is provided by comparison of the composition of micromanganese nodules, separated from one of these clays, with that of manganese nodules from the Pacific Ocean. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_854691 |
| institution | PANGAEA |
| language | en |
| publishDate | 1961 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 3, page 264), Composition of a manganese micronodule found in a fossil red clay bed from Western Timor El Wakeel, S K Riley, J P Aluminium oxide; Barium oxide; Calcium oxide; Carbon dioxide; Cobalt oxide; Copper(II) oxide; DEPTH, sediment/rock; Description; Flame photometry; Gallium oxide; Identification; Iron oxide, Fe2O3; Lead oxide; Magnesium oxide; Manganese oxide; Molybdenum trioxide; Nickel oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Noil_Tobee_M; Noni river, Timor; Oxygen, gas; Phosphorus pentoxide; Potassium oxide; Silicon dioxide; Sodium oxide; Spectrophotometric; Strontium oxide; Tin dioxide; Titanium dioxide; Vanadium oxide; Water in rock; Wet chemistry; Zinc oxide; Zirconium dioxide Chemical analyses are presented for two Cretaceous clays from Noil Tobee, Timor. Mineralogical examination has shown that they consist principally of quartz, feldspar, illite and chlorite, together with minor amounts of montmorillonite. Both chemically and mineralogically the clays are very similar to the recent argillaceous deep-sea sediments of the Pacific and Indian Oceans, which confirms Molengraaff's theory (1921) that they are of deep-sea origin. Further confirmation of this theory is provided by comparison of the composition of micromanganese nodules, separated from one of these clays, with that of manganese nodules from the Pacific Ocean. |
| title | (Table 3, page 264), Composition of a manganese micronodule found in a fossil red clay bed from Western Timor |
| topic | Aluminium oxide; Barium oxide; Calcium oxide; Carbon dioxide; Cobalt oxide; Copper(II) oxide; DEPTH, sediment/rock; Description; Flame photometry; Gallium oxide; Identification; Iron oxide, Fe2O3; Lead oxide; Magnesium oxide; Manganese oxide; Molybdenum trioxide; Nickel oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Noil_Tobee_M; Noni river, Timor; Oxygen, gas; Phosphorus pentoxide; Potassium oxide; Silicon dioxide; Sodium oxide; Spectrophotometric; Strontium oxide; Tin dioxide; Titanium dioxide; Vanadium oxide; Water in rock; Wet chemistry; Zinc oxide; Zirconium dioxide |
| url | https://doi.org/10.1594/PANGAEA.854691 |