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  • 1
    Publikationsdatum: 2024-01-09
    Schlagwort(e): 181-1121B; Age, dated; Age, dated standard deviation; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Growth rate; Joides Resolution; Leg181; Nodule, radius; Nodules growth rate, standard deviation; Nodules growth span; Ocean Drilling Program; ODP; Sample code/label; South Pacific Ocean; Standard deviation
    Materialart: Dataset
    Format: text/tab-separated-values, 50 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    Publikationsdatum: 2024-01-09
    Schlagwort(e): 181-1121B; Accelerator mass spectrometry (AMS); Beryllium-10; Beryllium-10/Beryllium-9; Beryllium-10/Beryllium-9, standard deviation; Beryllium-9; Comment; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Fraction; ICP-OES, Inductively coupled plasma - optical emission spectrometry; Joides Resolution; Leg181; Ocean Drilling Program; ODP; Sample code/label; South Pacific Ocean
    Materialart: Dataset
    Format: text/tab-separated-values, 325 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    Publikationsdatum: 2024-01-09
    Schlagwort(e): 181-1121B; Amphibole; Barite; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Feldspar; Joides Resolution; Kaolinite; Leg181; Mica; Ocean Drilling Program; ODP; Plagioclase; Quartz; Sample code/label; Silica, amorphous; South Pacific Ocean; X-ray diffraction (XRD)
    Materialart: Dataset
    Format: text/tab-separated-values, 63 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
    Publikationsdatum: 2024-01-09
    Schlagwort(e): 181-1121B; Accelerator mass spectrometry (AMS); Beryllium-10; Beryllium-10/Beryllium-9; Beryllium-10/Beryllium-9, standard deviation; Beryllium-9; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; ICP-OES, Inductively coupled plasma - optical emission spectrometry; Insoluble residue; Joides Resolution; Leg181; Number; Ocean Drilling Program; ODP; Range; Range, maximum; Range, minimum; Sample code/label; South Pacific Ocean
    Materialart: Dataset
    Format: text/tab-separated-values, 199 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
    Publikationsdatum: 2024-01-09
    Schlagwort(e): 181-1121B; Calculated; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; Duration; Joides Resolution; Leg181; Ocean Drilling Program; ODP; Sedimentation rate; Sedimentation rate, standard deviation; South Pacific Ocean
    Materialart: Dataset
    Format: text/tab-separated-values, 35 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
    Publikationsdatum: 2024-01-09
    Schlagwort(e): 181-1121B; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Grain size, mean; Joides Resolution; Leg181; Mode, grain size; Ocean Drilling Program; ODP; Particle size analyser; Sample code/label; Sand; Silt; Size fraction 〈 0.002 mm, clay; South Pacific Ocean
    Materialart: Dataset
    Format: text/tab-separated-values, 160 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 7
    Publikationsdatum: 2024-01-09
    Schlagwort(e): 181-1121B; Age, standard deviation; Age model; Age model, optional; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg181; Ocean Drilling Program; ODP; Sample code/label; South Pacific Ocean
    Materialart: Dataset
    Format: text/tab-separated-values, 148 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 8
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Graham, I J; Carter, Robert M; Ditchburn, R G; Zondervan, A (2004): Chronostratigraphy of ODP 181, Site 1121 sediment core (Southwest Pacific Ocean), using 10Be/9Be dating of entrapped ferromanganese nodules. Marine Geology, 205(1-4), 227-247, https://doi.org/10.1016/S0025-3227(04)00025-8
    Publikationsdatum: 2024-01-09
    Beschreibung: A 10Be/9Be-based chronostratigraphy has been determined for ODP 181, Site 1121 sediment core, recovered from the foot of the Campbell Plateau, Southwest Pacific Ocean. This core was drilled through the Campbell 'skin drift' in ca. 4500 m water depth on the mid-western margin of the extensive Campbell Nodule Field, beneath the flow of the major cold-water Deep Western Boundary Current (DWBC). In the absence of detailed biostratigraphy, beryllium isotopes have provided essential time information to allow palaeo-environmental interpretation to be undertaken on the upper 7 m of the core. Measured 10Be/9Be ratios of sediment, and of ferromanganese nodules entrapped in the sediment, decrease systematically with depth in the core, in accordance with radioactive decay. However, the 10Be/9Be data diverge from ca. 3 m below the seafloor (mbsf) to the top of the core, giving rise to several possible geochronological models. The preferred model assumes that the measured 10Be/9Be ratios of the nodule rims reflect initial 10Be/9Be ratios equivalent to contemporary seawater, and that these can be used to derive the true age of the sediment where the nodules occur. The nodule rim ages can be then used to interpret the sediment 10Be/9Be data, which indicate an overall age to ca. 7 mbsf of ca. 17.5 Ma. The derived chronology is consistent with diatom biostratigraphy, which indicates an age of 2.2-3.6 Ma at 1 mbsf. Calculated sedimentation rates range from 8 to 95 cm m.y.**-1, with an overall rate to 7 mbsf of ca. 39 cm m.y.**-1. The lowest rates generally coincide with the occurrence of entrapped nodules, and reflect periods of increased bottom current flow causing net sediment loss. Growth rates of individual nodules decrease towards the top of the sediment core, similar to the observed decrease in growth rate from core to rim of seafloor nodules from the Campbell Nodule Field. This may be related to an overall increase in the vigour of the DWBC from ca. 10 Ma to the present.
    Schlagwort(e): 181-1121; COMPCORE; Composite Core; Joides Resolution; Leg181; Ocean Drilling Program; ODP; South Pacific Ocean
    Materialart: Dataset
    Format: application/zip, 7 datasets
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  • 9
    Digitale Medien
    Digitale Medien
    Springer
    Journal of radioanalytical and nuclear chemistry 159 (1992), S. 267-279 
    ISSN: 1588-2780
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Chemie und Pharmazie , Energietechnik
    Notizen: Abstract We give a new general method of separation of the title radionuclides, using ferric hydroxide precipitations, cation exchange chromatography followed by anion exchange for U, further cation exchange for Pa and direct elution for Th. Electrodeposition for all three elements is from sulfate medium. Yields for Pa, Th, Pa, U are mostly about 98%. Matrices analyzed include calcite, dolomite, phosphorite, sediments, organic material, and mineral fractions from rock.
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
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  • 10
    Digitale Medien
    Digitale Medien
    Springer
    Journal of radioanalytical and nuclear chemistry 189 (1995), S. 115-125 
    ISSN: 1588-2780
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Chemie und Pharmazie , Energietechnik
    Notizen: Abstract Dating rocks using226Ra/230Th isochrons demands radiochemical purification of radium and thorium. This paper presents an improved method. Rocks are solubilised by nitric/nydrofluoric digestion followed by dissolution of insoluble fluorides by boric/nitric acids, and Th is extracted by passing the 8M nitric solution through an anion column in nitrate form. The eluant contains Ra and Ba which are precipitated as sulphate and redissolved in alkaline EDTA. Complete separation of Ba and Ra from sulphate is on an AG 1×8 anion column in EDTA form, which was found better than the chloride form. The Ba+Ra is separated on an AG 50W×8 cation column, and uses CDTA as an eluant for Ba. Careful pH control is essential. Ra elutes later with EDTA or 4M HCl and is precipitated with 125 μg barium as sulphate to yield a source suitable for α-spectrometry, or further treated to electroplate the Ra. The yield tracers used are228Th and224Ra. Because the sample contains natural224Ra a correction must be applied, calculated from the amount of natural232Th in the Th spectrum. Th may be precipitated with 100 μg of ferric iron and gives a spectrometry-quality source, but further purification and electrodeposition was found to be preferable. Variations on the method for the case of analysis of calcium-rich fish otoliths are described.
    Materialart: Digitale Medien
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