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Trace-element study and age dating of zircon from chromitites of the Bushveld Complex (South Africa) |
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| Authors: | Marina Yudovskaya Judith Kinnaird Anthony J Naldrett Nickolay Rodionov Anton Antonov Sergey Simakin Dmitry Kuzmin |
| Institution: | 1. Economic Geology Research Institute, University of the Witwatersrand, Pvt Bag 3, Wits, 2050, South Africa 6. Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry (IGEM RAS), 35 Staromonetny, Moscow, 119017, Russia 2. Centre of Isotopic Research, Russian Research Geological Institute (VSEGEI), 74 Sredny Pr., Saint-Petersburg, 199106, Russia 3. Institute of Microelectronics and Informatics (IMI RAS), 3 Krasnoborskaya St., Yaroslavl, 150051, Russia 4. Max-Planck-Institut für Chemie, Abteilung Biogeochemie, 55020, Mainz, Germany 5. V.S. Sobolev Institute of Geology and Mineralogy (IGM SB RAS), 3 Koptyuga Ave., Novosibirsk, 630090, Russia |
| Abstract: | The layered Bushveld Complex hosts a number of chromitite layers, which were found to contain significant amounts of zircon grains compared with adjacent silicate rocks. Cathodoluminescent-dark, partially metamict cores and transparent rims of composite zircon grains were analyzed for trace elements with SIMS and LA-ICPMS techniques. The cores are enriched in REE, Y, Th and U and are characterized by distinctly flatter REE patterns in contrast to those of the rims and transparent homogenous crystals. Zircon from the different stratigraphic units has specific Th/U ratios, the highest of which (1.5–4) occurs in a Merensky Reef zircon core. The Ti content of Bushveld zircon ranges from 12 to 52 ppm correlating to a crystallization temperature range of 760–930 °C. The geochemical characteristics of the first zircon generation are consistent with its high-temperature crystallization as the first major U, Th and REE acceptor from a highly-evolved residue of the high-Mg basalt magma, whereas the rims and coreless crystals have crystallized from percolating intercumulus liquid of new influx of the same magma. U-Pb SHRIMP dating of zircon cores and rims does not reveal a distinguishable difference between their ages indicating the absence of inherited zircon. Concordia ages of 2,051?±?9 Ma (2σ, MSWD?=?0.1) and 2,056?±?5 Ma (2σ, MSWD?=?0.05) for zircons from the Merensky Reef and the Upper Platreef located equally near the top of the Critical Zone are in agreement with published ages for the Merensky Reef. Zircon from the deeper-seated Lower Group, Middle Group and Lower Platreef chromitites yields younger concordia ages that may reflect prolonged late-stage volatile activity. |
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