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The study analyzes the sequence stratigraphic context of the Middle Jurassic Gypsum Spring Formation in Wyoming, focusing on its extensive basin-margin evaporites. The formation exhibits a variety of depositional environments and facies, indicating a complex history of gypsum and carbonate deposition influenced by climatic and geological factors. The findings suggest that the extensive evaporites were primarily formed from continental brines in a large desert mudflat setting, rather than from a narrow evapo

Author

elisepapke

Language

EN