FN Archimer Export Format
PT J
TI Hydrothermal fluid flow triggered by an earthquake in Iceland
BT 
AF Geoffroy, Laurent
   Dorbath, Catherine
   Ágústsson, Kristján
   Kristjánsdóttir, Sigríður
   Flóvenz, Ólafur G.
   Doubre, Cécile
   Gudmundsson, Ólafur
   Barreyre, Thibaut
   Bazin, Sara
   Franco, Aurore
AS 1:1;2:2;3:3;4:3;5:3;6:2;7:4;8:5;9:1;10:1;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;
C1 IUEM, CNRS, University of Western Britany, Brest, France
   EOST, CNRS, Université de Strasbourg, Strasbourg, France
   Iceland GeoSurvey, Reykjavik, Iceland
   Uppsala University, Uppsala, Sweden
   Centre of Deep-Sea Research, University of Bergen, Bergen, Norway
C2 UBO, FRANCE
   CNRS, FRANCE
   ICELAND GEOSURVEY, ICELAND
   UNIV UPPSALA, SWEDEN
   UNIV BERGEN, NORWAY
UM GEO-OCEAN
IN WOS Cotutelle UMR
   DOAJ
   copubli-france
   copubli-europe
IF 7.9
TC 1
UR https://archimer.ifremer.fr/doc/00755/86691/92136.pdf
   https://archimer.ifremer.fr/doc/00755/86691/92137.pdf
LA English
DT Article
AB Microearthquake hypocenters were analyzed in the Krýsuvík geothermal area in SW-Iceland with data taken from two consecutive passive seismic surveys, 2005 and 2009. Five years prior to the 2005 survey, this area was struck by an earthquake initiating a major top-to-bottom fluid migration in the upper crust. We observe from our surveys a complex bottom-to-top migration of seismicity with time following this fluid penetration, suggesting the migration of a pore pressure front controlled by the upper-crust fracture system. We interpret these data as the time and space development of high-temperature hydrothermal cells from a deep upper crustal fluid reservoir in the supercritical field. These results provide an insight into the coupling mechanisms between active tectonics and fluid flow in upper-crustal extensional systems with high thermal flux. 
PY 2022
PD MAR
SO Communications Earth & Environment
SN 2662-4435
PU Springer Science and Business Media LLC
VL 3
IS 1
UT 000767365500003
DI 10.1038/s43247-022-00382-0
ID 86691
ER

EF