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Eocene to Oligocene Provenance and Drainage in Extensional Basins of Southwest Montana and East-central Idaho: Evidence From Detrital Zircon Populations in the Renova Formation and Equivalent Strata
Middle Eocene to Early Miocene sedimentary rocks in southwest Montana and east-central Idaho were deposited within an actively extending north-trending rift system (Cabbage Patch beds and Medicine Lodge beds) and a broad depositional basin on the eastern flank of this rift (Renova Formation). Distin
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