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Archaean flow-top alteration zones formed initially in a low-temperature sulphate-rich environment

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Filamentous microfossils from the 3,500 million year old Onverwacht Group, Barberton Mountain Land, South Africa

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Rb–Sr and Sm–Nd isotope geochmistry of cherts from the Onverwacht Group (3.5AE), South Africa

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10.1016/0012-821x(84)90112-2 · 1984 · External reference

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