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Provenance of Eocene to Oligocene Sandstones of Southwest Montana: Evidence From Detrital Zircons
Late Paleogene sedimentary rocks in southwest Montana and eastern Idaho were deposited in syn-extensional basins of a north-trending Paleogene rift system' (Medicine Lodge and Cabbage Patch beds) and a broad depositional basin (Renova Formation) to the east of the rift. Amagmatic Paleogene rifting i
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