Akademik Veri Yönetim Sistemi
PURE AND APPLIED GEOPHYSICS, cilt.169, sa.4, ss.659-675, 2012 (SCI-Expanded)
A temporary earthquake station network of 11 seismological recorders was operated in the Bursa region, south of the Marmara Sea in the northwest of Turkey, which is located at the southern strand of the North Anatolian Fault Zone (NAFZ). We located 384 earthquakes out of a total of 582 recorded events that span the study area between 28.50-30.00 degrees E longitudes and 39.75-40.75 degrees N latitudes. The depth of most events was found to be less than 29 km, and the magnitude interval ranges were between 0.3 <= M-L <= 5.4, with RMS less than or equal to 0.2. Seismic activities were concentrated southeast of Uludag Mountain (UM), in the Kestel-Igdir area and along the Gemlik Fault (GF). In the study, we computed 10 focal mechanisms from temporary and permanents networks. The predominant feature of the computed focal mechanisms is the relatively widespread near horizontal northwest-southeast (NW-SE) T-axis orientation. These fault planes have been used to obtain the orientation and shape factor (R, magnitude stress ratio) of the principal stress tensors (sigma(1), sigma(2), sigma(3)). The resulting stress tensors reveal sigma(1) closer to the vertical (oriented NE-SW) and sigma(2), sigma(3) horizontal with R = 0.5. These results confirm that Bursa and its vicinity could be defined by an extensional regime showing a primarily normal to oblique-slip motion character. It differs from what might be expected from the stress tensor inversion for the NAFZ. Different fault patterns related to structural heterogeneity from the north to the south in the study area caused a change in the stress regime from strike-slip to normal faulting.