FN Archimer Export Format
PT J
TI Creep-dilatancy development at a transform plate boundary
BT 
AF Sultan, Nabil
   Murphy, Shane
   Riboulot, Vincent
   Géli, Louis
AS 1:1;2:1;3:1;4:1;
FF 1:PDG-REM-GEOOCEAN-ALMA;2:PDG-REM-GEOOCEAN-ALMA;3:PDG-REM-GEOOCEAN-ALMA;4:PDG-REM-GEOOCEAN-ALMA;
C1 Geo-Ocean UMR6538, Ifremer, CNRS, UBO, UBS, 29280, Plouzané, France
C2 IFREMER, FRANCE
SI BREST
SE PDG-REM-GEOOCEAN-ALMA
UM GEO-OCEAN
IN WOS Ifremer UMR
   DOAJ
IF 16.6
TC 2
UR https://archimer.ifremer.fr/doc/00765/87664/93158.pdf
   https://archimer.ifremer.fr/doc/00765/87664/93159.pdf
   https://archimer.ifremer.fr/doc/00765/87664/93160.pdf
LA English
DT Article
CR MARMARA
   MARSITECRUISE
BO Le Suroît
   Pourquoi pas ?
AB How tectonic plates slip slowly and episodically along their boundaries, is a major, open question in earthquake science. Here, we use offshore in-situ sediment pore-pressure acquired in the proximity of the active offshore Main Marmara Fault and onshore geodetic time-series data set from a single GPS station to demonstrate the pore-pressure/deformation coupling during a 10-month slow-slip event. We show that pore pressure fluctuations are the expression of hydro-mechanical process affecting the deep seismogenic zone and indicate that small disturbances in geodetic data may have important meaning in terms of transient deformations. These results have major implications in understanding the spatial impact of slow-slip processes and their role in earthquake cycles. We demonstrate that piezometers measuring along a transform fault can help define the time scale regulating the coupling between slow-slip events and earthquake nucleation process. 
PY 2022
PD APR
SO Nature Communications
SN 2041-1723
PU Springer Science and Business Media LLC
VL 13
IS 1
UT 000781498700013
DI 10.1038/s41467-022-29558-0
ID 87664
ER

EF