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  • 1
    Publication Date: 2023-05-12
    Keywords: Belssbank; CIPW Norm; Diopside; Event label; Ilmenite; Kaalvallei; Magnetite; MULT; Multiple investigations; Nepheline; Olivine; ORDINAL NUMBER; Plagioclase; Pyroxene; Sample code/label; South Africa; Total
    Type: Dataset
    Format: text/tab-separated-values, 54 data points
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  • 2
    Publication Date: 2023-05-12
    Keywords: Belssbank; Calculated; Chromium(III) oxide; Event label; Garnet; Iron 2+/Iron total ratio; Iron 2+/Iron total ratio, standard deviation; Iron oxide, FeO; Kaalvallei; MULT; Multiple investigations; ORDINAL NUMBER; Pyroxene; Sample code/label; Sodium oxide; South Africa; Standard deviation; Temperature, calculated; Δδ18O; δ18O; δ18O, standard deviation; δ56/54Fe; δ56/54Fe, standard deviation; δ57/54Fe; δ57/54Fe, standard deviation; δ57/56Fe; δ57/56Fe, standard deviation; δ57Fe; δ57Fe, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 226 data points
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  • 3
    Publication Date: 2023-05-12
    Keywords: Aluminium oxide; Aluminium oxide, standard deviation; Belssbank; Calcium oxide; Calcium oxide, standard deviation; Electron microprobe (EMP); Elements, total; Elements, total, standard deviation; Event label; Iron oxide, FeO; Iron oxide, FeO, standard deviation; Kaalvallei; Magnesium oxide; Magnesium oxide, standard deviation; Manganese oxide; Manganese oxide, standard deviation; Mineral name; MULT; Multiple investigations; Nickel oxide; Nickel oxide, standard deviation; ORDINAL NUMBER; Potassium oxide; Potassium oxide, standard deviation; Sample amount; Sample code/label; Silicon dioxide; Silicon dioxide, standard deviation; Sodium oxide; Sodium oxide, standard deviation; South Africa; Titanium dioxide; Titanium dioxide, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 250 data points
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  • 4
    Publication Date: 2023-05-12
    Keywords: Belssbank; Event label; Kaalvallei; MULT; Multiple investigations; ORDINAL NUMBER; Sample code/label; Sample comment; South Africa; δ18O; δ18O, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 52 data points
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  • 5
    Publication Date: 2023-07-10
    Keywords: Arsenic; Barium; Belssbank; Beryllium; Boron; Caesium; Cerium; Chromium; Cobalt; Copper; Dysprosium; Erbium; Europium; Event label; Gadolinium; Gallium; Germanium; Hafnium; Holmium; Kaalvallei; LA-ICP-MS, Laser-ablation inductively coupled plasma mass spectrometer; Lanthanum; Lead; Lithium; Lutetium; Mineral name; Molybdenum; MULT; Multiple investigations; Neodymium; Nickel; Niobium; ORDINAL NUMBER; Phosphorus; Potassium; Praseodymium; Rubidium; Samarium; Sample amount; Sample code/label; Scandium; South Africa; Strontium; Tantalum; Terbium; Thorium; Thulium; Uranium; Vanadium; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 540 data points
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  • 6
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    Unknown
    PANGAEA
    In:  Supplement to: Portner, Ryan A; Daczko, Nathan R; Murphy, Melissa J; Pearson, Norman J (2011): Enriching mantle melts within a dying mid-ocean spreading ridge: Insights from Hf-isotope and trace element patterns in detrital oceanic zircon. Lithos, 126(3-4), 355-368, https://doi.org/10.1016/j.lithos.2011.07.017
    Publication Date: 2023-11-11
    Description: Oceanic zircon trace element and Hf-isotope geochemistry offers a means to assess the magmatic evolution of a dying spreading ridge and provides an independent evaluation of the reliability of oceanic zircon as an indicator of mantle melting conditions. The Macquarie Island ophiolite in the Southern Ocean provides a unique testing ground for this approach due to its formation within a mid-ocean ridge that gradually changed into a transform plate boundary. Detrital zircon recovered from the island records this change through a progressive enrichment in incompatible trace elements. Oligocene age (33-27 Ma) paleo-detrital zircon in ophiolitic sandstones and breccias interbedded with pillow basalt have trace element compositions akin to a MORB crustal source, whereas Late Miocene age (8.5 Ma) modern-detrital zircon collected from gabbroic colluvium on the island have highly enriched compositions unlike typical oceanic zircon. This compositional disparity between age populations is not complimented by analytically equivalent eHf data that primarily ranges from 14 to 13 for sandstone and modern-detrital populations. A wider compositional range for the sandstone population reflects a multiple pluton source provenance and is augmented by a single cobble clast with eHf equivalent to the maximum observed composition in the sandstone (~17). Similar sandstone and colluvium Hf-isotope signatures indicate inheritance from a similar mantle reservoir that was enriched from the depleted MORB mantle average. The continuity in Hf-isotope signature relative to trace element enrichment in Macquarie Island zircon populations, suggests the latter formed by reduced partial melting linked to spreading-segment shortening and transform lengthening along the dying spreading ridge.
    Keywords: Age, dated; Age, dated standard deviation; Age, Uranium-Lead; Area/locality; Calcium-43; Central-eastern Macquarie Island coastal escarpment; Central-western Macquarie Island coastal escarpment; Cerium/Cerium ratio; Cerium-140; Correlation coefficient, isotope ratio error; CP1-5; DLP1B-5A; Dysprosium-163; Electron microprobe (EMP); Erbium-166; Europium-151; Europium anomaly; Event label; Gadolinium-157; Geological sample; GEOS; Hafnium-178; Hafnium oxide; Holmium-165; LA-ICP-MS, Laser-ablation inductively coupled plasma mass spectrometer; Lanthanum-139; Latitude of event; Lead-204; Lead-206; Lead-206/Uranium-238, error; Lead-206/Uranium-238 ratio; Lead-207; Lead-207/Lead-206, standard error; Lead-207/Lead-206 ratio; Lead-207/Uranium-235, error; Lead-207/Uranium-235 ratio; Lead-208; Lead-208/Thorium-232, error; Lead-208/Thorium-232 ratio; Location of event; Longitude of event; Lutetium-175; Lutetium-176/Hafnium-177; Lutetium-176/Hafnium-177, error; MACA; MM1-1; MP1-4; MW6-2; Neodymium-146; Niobium-93; Northern Macquarie island plateau; Northwestern Macquarie Island coast; Praseodymium-141; Samarium-147; Sample code/label; Silicon dioxide; Southwest Macquarie Island coast; SW2-2; Tantalum-181; Temperature, technical; Temperature, technical, standard deviation; Terbium-159; Thorium/Uranium ratio; Thorium-232; Thulium-169; Titanium-49; Uranium/Ytterbium ratio; Uranium-238; Ytterbium/Samarium ratio; Ytterbium-173; Ytterbium-176/Hafnium-177; Yttrium-89; Yttrium oxide; Zirconium dioxide; ε-Hafnium; ε-Hafnium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 9767 data points
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  • 7
    Publication Date: 2024-01-09
    Keywords: 111-504B; 148-504B; 83-504B; Chromium(III) oxide; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Iron 2+/Iron total ratio; Iron oxide, FeO; Joides Resolution; Leg111; Leg148; Leg83; North Pacific Ocean; Ocean Drilling Program; ODP; Rock type; Sample code/label; δ18O; δ56/54Fe; δ56/54Fe, standard deviation; δ57/54Fe; δ57/54Fe, standard deviation; δ57/56Fe; δ57/56Fe, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 83 data points
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  • 8
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    Unknown
    PANGAEA
    In:  Supplement to: Williams, Helen M; Nielsen, Sune G; Renac, Christope; Griffin, William L; O'Reilley, Suzanne Y; McCammon, Catherine A; Pearson, Norman J; Viljoen, Fanus; Alt, Jeffrey C; Halliday, Alex N (2009): Fractionation of oxygen and iron isotopes by partial melting processes: Implications for the interpretation of stable isotope signatures in mafic rocks. Earth and Planetary Science Letters, 283(1-4), 156-166, https://doi.org/10.1016/j.epsl.2009.04.011
    Publication Date: 2024-01-09
    Description: Recycling of oceanic crust into the deep mantle via subduction is a widely accepted mechanism for creating compositional heterogeneity in the upper mantle and for explaining the distinct geochemistry of mantle plumes. The oxygen isotope ratios (d18O) of some ocean island basalts (OIB) span values both above and below that of unmetasomatised upper mantle (5.5 ± 0.4 per mil) and provide support for this hypothesis, as it is widely assumed that most variations in d18O are produced by near-surface low-temperature processes. Here we show a significant linear relationship between d18O and stable iron isotope ratios (d57Fe) in a suite of pristine eclogite xenoliths. The d18O values of both bulk samples and garnets range from values within error of normal mantle to significantly lighter values. The observed range and correlation between d18O and d57Fe is unlikely to be inherited from oceanic crust, as d57Fe values determined for samples of hydrothermally altered oceanic crust do not differ significantly from the mantle value and show no correlation with d18O. It is proposed that the correlated d57Fe and d18O variations in this particular eclogite suite are predominantly related to isotopic fractionation by disequilibrium partial melting although modification by melt percolation processes cannot be ruled out. Fractionation of Fe and O isotopes by removal of partial melt enriched in isotopically heavy Fe and O is supported by negative correlations between bulk sample d57Fe and Cr content and bulk sample and garnet d18O and Sc contents, as Cr and Sc are elements that become enriched in garnet- and pyroxene-bearing melt residues. Melt extraction could take place either during subduction, where the eclogites represent the residues of melted oceanic lithosphere, or could take place during long-term residence within the lithospheric mantle, in which case the protoliths of the eclogites could be of either crustal or mantle origin. This modification of both d57Fe and d18O by melting processes and specifically the production of low-d18O signatures in mafic rocks implies that some of the isotopically light d18O values observed in OIB and eclogite xenoliths may not necessarily reflect near-surface processes or components.
    Keywords: Deep Sea Drilling Project; DSDP; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 9
    ISSN: 1751-908X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: This paper describes a technique for the preparation of a titanite (CaTiSiO5) glass calibration material for use in in situ microanalysis of major, minor, and trace elements in geological materials. The starting composition was a titanite matrix doped with minor and trace elements at ∼ 200 μg g-1. The elements Sc, Y, REEs, Th and U were added in the form of nitrates in solution, and the elements V, Cr, Mn, Fe, Co, Ni, Zr, Nb, Hf and W were added as solid oxides. The synthetic titanite glass was produced by direct fusion by resistance heating in graphite electrodes at 1600-1700 °C, and quenched in air. Backscattered electron images indicate good homogeneity, with no signs of separate phases or vesicles, and analysis of the major elements Ca, Ti and Si by electron microprobe showed relative standard deviations between 0.5 and 0.7%, based on six independent measurements. Deviations from nominal concentrations for Ca, Si and Ti were measured to -1.2, -3.3 and -0.8%, respectively. The homogeneity of the trace elements in the glass was assessed by LA-ICP-MS analyses, using NIST SRM 610, 612 and 616 as external calibrators, and Ca as the internal standard element. Determinations were made both with a quadrupole mass spectrometer and a sector field instrument, and both raster and spot modes of analysis were used. For the majority of doped elements, precision was better than 10%, and relative deviations from nominal values were, with few exceptions, between 5 and 10%.
    Type of Medium: Electronic Resource
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  • 10
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Abyssal peridotites are assumed to represent the mantle residue of mid-ocean-ridge basalts (MORBs). However, the osmium isotopic compositions of abyssal peridotites and MORB do not appear to be in equilibrium, raising questions about the cogenetic relationship between those two reservoirs. ...
    Type of Medium: Electronic Resource
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