(Table 1a, page 321) Chemical composition of Fe-Mn rich layers in the sediments probed during DSDP Leg 54 (Holes 419, 420, 424, 424A, 427)
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
1980
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| _version_ | 1867172336037265408 |
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| author | Schrader, Ed L Furbish, William J Mattey, David P May, J A |
| author_facet | Schrader, Ed L Furbish, William J Mattey, David P May, J A |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Thirty selected samples of pelagic and hydrothermal sediments retrieved on DSDP Leg 54 were chemically analyzed for major and minor oxide concentrations. Additionally, 11 samples of lithified carbonate sediments were petrologically studied. The pelagic sediments, which are described as foraminiferal biomicrite, were found to be generally higher in Fe and Zn, similar in Co content, and lower in Cu content, than the average Pacific pelagic sediments. Mineralogically, these samples are composed principally of calcite with minor amounts of quartz and clays. Hydrothermal sediments from Site 424 are divisible into three classes: (1) silica-rich, iron-poor smectites; (2) silica-poor, iron-rich mixtures of smectites and oxides; and (3) silica-poor, iron-rich materials, comprising mainly amorphous manganese oxides. Thus, two chemically distinct hydrothermal phases are recognizable: Class 1, iron-rich smectites, and Class 3, Mn-rich oxides and oxyhydroxides. Dolomite and pyrite were identified in X-ray diffraction studies of samples from Site 427. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_873019 |
| institution | PANGAEA |
| language | en |
| publishDate | 1980 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 1a, page 321) Chemical composition of Fe-Mn rich layers in the sediments probed during DSDP Leg 54 (Holes 419, 420, 424, 424A, 427) Schrader, Ed L Furbish, William J Mattey, David P May, J A 54-419; 54-420; 54-424; 54-424A; 54-427; Atomic absorption spectrometry (AAS); Cobalt; Copper; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Iron; Leg54; Manganese; Molybdenum; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/MOUND; North Pacific/SEDIMENT POND; North Pacific/TROUGH; Sediment type; X-ray fluorescence (XRF); Zinc Thirty selected samples of pelagic and hydrothermal sediments retrieved on DSDP Leg 54 were chemically analyzed for major and minor oxide concentrations. Additionally, 11 samples of lithified carbonate sediments were petrologically studied. The pelagic sediments, which are described as foraminiferal biomicrite, were found to be generally higher in Fe and Zn, similar in Co content, and lower in Cu content, than the average Pacific pelagic sediments. Mineralogically, these samples are composed principally of calcite with minor amounts of quartz and clays. Hydrothermal sediments from Site 424 are divisible into three classes: (1) silica-rich, iron-poor smectites; (2) silica-poor, iron-rich mixtures of smectites and oxides; and (3) silica-poor, iron-rich materials, comprising mainly amorphous manganese oxides. Thus, two chemically distinct hydrothermal phases are recognizable: Class 1, iron-rich smectites, and Class 3, Mn-rich oxides and oxyhydroxides. Dolomite and pyrite were identified in X-ray diffraction studies of samples from Site 427. |
| title | (Table 1a, page 321) Chemical composition of Fe-Mn rich layers in the sediments probed during DSDP Leg 54 (Holes 419, 420, 424, 424A, 427) |
| topic | 54-419; 54-420; 54-424; 54-424A; 54-427; Atomic absorption spectrometry (AAS); Cobalt; Copper; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Iron; Leg54; Manganese; Molybdenum; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/MOUND; North Pacific/SEDIMENT POND; North Pacific/TROUGH; Sediment type; X-ray fluorescence (XRF); Zinc |
| url | https://doi.org/10.1594/PANGAEA.873019 |