@article{FaithfullTimmermanUptonetal.2012,
  author    = {Faithfull, J. W. and Timmerman, Martin Jan and Upton, B. G. J. and Rumsey, M. S.},
  title     = {Mid-Eocene renewal of magmatism in NW Scotland the Loch Roag Dyke, outer hebrides},
  series = {Journal of the Geological Society},
  volume    = {169},
  journal   = {Journal of the Geological Society},
  number    = {2},
  publisher = {Geological Soc. Publ. House},
  address   = {Bath},
  issn      = {0016-7649},
  doi       = {10.1144/0016-76492011-117},
  pages     = {115 -- 118},
  year      = {2012},
  abstract  = {Amonchquite dyke, in the vicinity of Loch Roag, Lewis, Outer Hebrides has an unusually enriched chemistry, and contains a unique assemblage of megacrysts and xenoliths from the lithosphere of the Hebridean craton. A Ar-40/Ar-39 plateau age of 45.2 +/- 0.2 Ma (2 sigma) of a phlogopite megacryst from the dyke overlaps an earlier reported K-Ar age, and confirms that the British Palaeogene Igneous Province extended into the Eocene. Similar late low-volume melts were erupted in the Eocene and Oligocene in West and East Greenland, suggesting that such late-stage magmatic rejuvenescence is a widespread feature across the North Atlantic Igneous Province.},
  language  = {en}
}