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| Format: | Dataset Open Access |
| Sprache: | en |
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PANGAEA
1983
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| Online-Zugang: | https://doi.org/10.1594/PANGAEA.811424 |
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| _version_ | 1867171815580762112 |
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| author | Weaver, Barry L Marsh, Nicholas G Tarney, J |
| author_facet | Weaver, Barry L Marsh, Nicholas G Tarney, J |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | The geochemistry of basalts recovered during Leg 72 is described with emphasis on trace elements. Only Hole 516F penetrated basement; the basalts recovered are plagioclase-phyric and olivine-phyric and pervasively altered. Chemically, the basalts from Hole 516F are rather uniform in composition. However, four distinct geochemical units can be recognized, although the chemistry of two of the units appears to be controlled by chemical mobility associated with alteration. The two less-altered units cannot be related by fractional crystallization processes. Hole 516F basalts have a trace element chemistry characteristic of T-type mid-ocean ridge basalt; rare-earth element patterns (as indicated by Ce/Y ratios) are mildly fractionated flight rare-earth element enriched), and a number of incompatible element ratios are close to chondritic. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_811424 |
| institution | PANGAEA |
| language | en |
| publishDate | 1983 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 1) Major and trace elements of basalts at DSDP Hole 72-516F Weaver, Barry L Marsh, Nicholas G Tarney, J 72-516F; Aluminium oxide; Barium; Calcium oxide; Cerium; Cerium/Yttrium ratio; Chromium; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Gallium; Glomar Challenger; Iron oxide, Fe2O3; Lanthanum; Lead; Leg72; Lithologic unit/sequence; Magnesium number; Magnesium oxide; Manganese oxide; Neodymium; Nickel; Niobium; Phosphorus pentoxide; Piece; Potassium oxide; Rubidium; Sample code/label; Silicon dioxide; Sodium oxide; South Atlantic/CONT RISE; Strontium; Thorium; Titanium/Zirconium ratio; Titanium dioxide; Total; Vanadium; X-ray fluorescence (XRF); Yttrium; Zinc; Zirconium; Zirconium/Niobium ratio The geochemistry of basalts recovered during Leg 72 is described with emphasis on trace elements. Only Hole 516F penetrated basement; the basalts recovered are plagioclase-phyric and olivine-phyric and pervasively altered. Chemically, the basalts from Hole 516F are rather uniform in composition. However, four distinct geochemical units can be recognized, although the chemistry of two of the units appears to be controlled by chemical mobility associated with alteration. The two less-altered units cannot be related by fractional crystallization processes. Hole 516F basalts have a trace element chemistry characteristic of T-type mid-ocean ridge basalt; rare-earth element patterns (as indicated by Ce/Y ratios) are mildly fractionated flight rare-earth element enriched), and a number of incompatible element ratios are close to chondritic. |
| title | (Table 1) Major and trace elements of basalts at DSDP Hole 72-516F |
| topic | 72-516F; Aluminium oxide; Barium; Calcium oxide; Cerium; Cerium/Yttrium ratio; Chromium; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Gallium; Glomar Challenger; Iron oxide, Fe2O3; Lanthanum; Lead; Leg72; Lithologic unit/sequence; Magnesium number; Magnesium oxide; Manganese oxide; Neodymium; Nickel; Niobium; Phosphorus pentoxide; Piece; Potassium oxide; Rubidium; Sample code/label; Silicon dioxide; Sodium oxide; South Atlantic/CONT RISE; Strontium; Thorium; Titanium/Zirconium ratio; Titanium dioxide; Total; Vanadium; X-ray fluorescence (XRF); Yttrium; Zinc; Zirconium; Zirconium/Niobium ratio |
| url | https://doi.org/10.1594/PANGAEA.811424 |