(Table 2, Page 270) Average chemical composition of manganese nodules and crust collected at different localities the Pacific Ocean
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
1977
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| _version_ | 1867168171698421760 |
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| author | Nohara, Masato |
| author_facet | Nohara, Masato |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Considerable regional variations in the chemical composition of manganese nodules from a wide range of the Pacific Ocean have been observed. These variations can be more exactly expressed in terms of inter-element relationships. In particular, Cu-Mn and Cu-Ni associations reveal that Cu content in pelagic nodules increases rapidly in proportion to those of Mn or Ni. In nodules from continental borderland and hemipelagic areas, even if Mn or Ni contents increase, that of Cu increases only slightly. It is suggested that the considerable chemical differences within individual nodules and between nodules from the same site, at a limited pelagic area where there is no marked change in depositional conditions of nodules, are due to the role of hydrolyzable trace elements in the formation of nodules. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_858503 |
| institution | PANGAEA |
| language | en |
| publishDate | 1977 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 2, Page 270) Average chemical composition of manganese nodules and crust collected at different localities the Pacific Ocean Nohara, Masato Aluminium; Atomic absorption spectrometry (AAS), Perkin-Elmer; Cobalt; Copper; Core; CORE; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; Geographical setting; GH76-2; GH76-2-D144; Hakuho-Maru; Hakurei-Maru (1974); Identification; Iron; KH67-5-34; KH67-5-40; KH-68-3; KH68-3-9-16-2; KH68-3-9-6; KH68-3-9-7; KH68-3-9-8; KH68-3-9-9; KH-68-4; KH68-4-33-2; KH68-4-41-2; KH-69-2; KH69-2-1-1; KH69-2-5-1; KH-71-1; KH71-1-3-3a; KH-71-5; KH71-5-12-3; KH71-5-15-3; KH71-5-20-3; KH-72-2; KH72-2-46; KH-76-2; KH76-32-2; Latitude of event; Lead; Longitude of event; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Number of subsamples; OKAD01; OKAD02; Pacific Ocean; Sediment type; SPac_1968-69_HH_170W; SPac_1971_HH_150-100W; Station 441; Titanium; Zinc Considerable regional variations in the chemical composition of manganese nodules from a wide range of the Pacific Ocean have been observed. These variations can be more exactly expressed in terms of inter-element relationships. In particular, Cu-Mn and Cu-Ni associations reveal that Cu content in pelagic nodules increases rapidly in proportion to those of Mn or Ni. In nodules from continental borderland and hemipelagic areas, even if Mn or Ni contents increase, that of Cu increases only slightly. It is suggested that the considerable chemical differences within individual nodules and between nodules from the same site, at a limited pelagic area where there is no marked change in depositional conditions of nodules, are due to the role of hydrolyzable trace elements in the formation of nodules. |
| title | (Table 2, Page 270) Average chemical composition of manganese nodules and crust collected at different localities the Pacific Ocean |
| topic | Aluminium; Atomic absorption spectrometry (AAS), Perkin-Elmer; Cobalt; Copper; Core; CORE; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; Geographical setting; GH76-2; GH76-2-D144; Hakuho-Maru; Hakurei-Maru (1974); Identification; Iron; KH67-5-34; KH67-5-40; KH-68-3; KH68-3-9-16-2; KH68-3-9-6; KH68-3-9-7; KH68-3-9-8; KH68-3-9-9; KH-68-4; KH68-4-33-2; KH68-4-41-2; KH-69-2; KH69-2-1-1; KH69-2-5-1; KH-71-1; KH71-1-3-3a; KH-71-5; KH71-5-12-3; KH71-5-15-3; KH71-5-20-3; KH-72-2; KH72-2-46; KH-76-2; KH76-32-2; Latitude of event; Lead; Longitude of event; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Number of subsamples; OKAD01; OKAD02; Pacific Ocean; Sediment type; SPac_1968-69_HH_170W; SPac_1971_HH_150-100W; Station 441; Titanium; Zinc |
| url | https://doi.org/10.1594/PANGAEA.858503 |