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Triassic Sherwood Sandstone Group

The Triassic Sherwood Sandstone Group is a geological formation primarily composed of sandstones and pebbly sandstones, with some conglomerate and minor mudstone and siltstone. It was deposited during the late Permian and Triassic periods, roughly 230 to 260 million years ago. The group is known for its varied depositional environments, including fluvial (river-dominated) and aeolian (wind-dominated) settings, and its potential as a geothermal aquifer.