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Seismicity distribution and locking depth along the Main Marmara Fault, Turkey
2016
Geochemistry Geophysics Geosystems
The seismicity along the Main Marmara Fault (MMF) below the Marmara Sea is analyzed during the 2007-2012 period to provide insights on the recent evolution of this important regional seismic gap. High precision locations show that seismicity is strongly varying along strike and depth providing fine details of the fault behavior that are inaccessible from geodetic observations. The activity strongly clusters at the regions of transition between basins. The Central basin shows significant
doi:10.1002/2015gc006120
fatcat:twkfle5yk5e7rebfn43wnapyym