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Investigating La Reunion hotspot from crust to core

Barruol, Guilhem, and Karin Sigloch (2013), Investigating La Reunion hotspot from crust to core, Eos, Transactions American Geophysical Union, 94(23), 205-207, doi:10.1002/2013EO230002.

Abstract
Whether volcanic intraplate hot spots are underlain by deep mantle plumes continues to be debated 40 years after the hypothesis was proposed by Morgan [1972]. Arrivals of buoyant plume heads may have been among the most disruptive agents in Earth's history, initiating continental breakup, altering global climate, and triggering mass extinctions. Further, with the temporary shutdown of European air traffic in 2010 caused by the eruption of Eyjafjallajökull, a geologically routine eruption in the tail end of the presumed Iceland plume, the world witnessed an intrusion of hot spot activity into modern-day life.
Further information
BibTeX
@article{id1853,
  author = {Guilhem Barruol and Karin Sigloch},
  journal = {Eos, Transactions American Geophysical Union},
  month = {jun},
  number = {23},
  pages = {205-207},
  title = {{Investigating La Reunion hotspot from crust to core}},
  volume = {94},
  year = {2013},
  url = {http://onlinelibrary.wiley.com/doi/10.1002/2013EO230002/abstract},
  doi = {10.1002/2013EO230002},
}
EndNote
%0 Journal Article
%A Barruol, Guilhem
%A Sigloch, Karin
%D 2013
%N 23
%V 94
%J Eos, Transactions American Geophysical Union
%P 205-207
%T Investigating La Reunion hotspot from crust to core
%U http://onlinelibrary.wiley.com/doi/10.1002/2013EO230002/abstract
%8 jun
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Printed 20. Mar 2019 04:13