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The tholeiitic series is a classification of subalkaline volcanic igneous rocks characterized by their iron-rich composition. These rocks, primarily basalts, contain plagioclase feldspar, augite, and often pigeonite or hypersthene, with little to no olivine. Tholeiitic basalts typically have a silica content between 45 and 63 percent.12

This series is commonly found along divergent plate boundaries, such as oceanic ridges, and can form extensive plateaus. Examples include the lavas of the Pacific Northwest, the Deccan in India, and the Paran\u00e1 Basin in South America. While often found underwater, tholeiitic lavas also erupt on land, as seen in regions like Iceland.123

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