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Strontium, neodymium, and lead isotopic evidence for the interaction of post-suhduction asthenospheric potassic mafic magmas of the Highwood Mountains, Montana, USA, with ancient Wyoming craton lithospheric mantle

Magmatic ProcessVolcanologyEngineeringMagmatismIgneous PetrogenesisLead Isotopic EvidenceGeologyGeochemistryCrust-mantle InteractionPetrologyEarth ScienceMantle GeochemistryHighwood MountainsTectonics