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The Eel Creek Formation, which crops out along the northeastern edge of the Archean Pilbara Craton in Western Australia, is a formerly undated, siliciclastic succession with a preserved thickness of at least 500m. Only a small portion of the basin is exposed at surface; the bulk of it is buried beneath Neoproterozoic and Phanerozoic basins. Two tuff samples from near the base of the succession have...
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