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FAULT INTERACTIONS IN THE SEA OF MARMARA PULL-APART (NORTH ANATOLIAN FAULT): EARTHQUAKE CLUSTERING AND PROPAGATING EARTHQUAKE SEQUENCES (2007)

Knowledge on large earthquakes (M 7.0), geology and fault kinematics is used to analyse conditions that favour isolated seismicity, clustered earthquakes or propagating sequencesalong the North Anatolian Fault (NAF) and the Sea of Marmara pull-apart.
Reference:
Geophys. J. Int. (2007) 171, 1185-1197
Organization:
Laboratoire de Tectonique, IPGP, CNRS-UMR 7578, 4, place Jussieu, 75252 Paris Cedex 05, France
Turkey
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