FN Archimer Export Format
PT J
TI Investigating La Réunion Hot Spot From Crust to Core
BT 
AF Barruol, Guilhem
   Sigloch, Karin
AS 1:1;2:2;
FF 1:;2:;
C1 GéoSciences Réunion, Université de La Réunion, Institut de Physique du Globe de Paris, Centre National de la Recherche Scientifique, Saint Denis de La Réunion, France
   Department of Earth and Environmental Sciences, Ludwig- Maximilians- Universität München, Munich, Germany
C2 UNIV LA REUNION, FRANCE
   UNIV MUNICH, GERMANY
TC 0
UR https://archimer.ifremer.fr/doc/00273/38465/36874.pdf
LA English
DT Article
CR MD 192 / RHUM-RUM
BO Marion Dufresne
AB 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.
PY 2013
PD JUL
SO Eos, Transactions American Geophysical Union
SN 00963941
PU Wiley-Blackwell
VL 94
IS 23
BP 205
EP 207
DI 10.1002/2013EO230002
ID 38465
ER

EF