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The Benmara region in the Northern Territory, Australia, hosts the Buddycurrawa Volcanics, a sequence of trachyte lavas and shallow-marine siliciclastic rocks. Carson et al. (2020) provide new geochronology data establishing an extrusion age constrained between ca. 1662 Ma and 1631 Ma. The data also describe hydrothermal features like 'white smoker' pipes and pervasive potassic alteration dated to ca. 1612–1323 Ma.
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