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Apatite (U–Th)/He and fission track data from profiles in western Scotland constrain the timing and magnitude of denudation during the early Cenozoic when the north Atlantic region was the site of intense magmatic activity related to the proto-Icelandic plume. Apatite helium ages vary from 77±8 to 265±27 Ma (±2σ) at Sgorr Dhonuill, Ballachulish, and from 104±10 Ma to 166±17 Ma at Clisham, Outer Hebrides...
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