Geometry and segmentation of the North Anatolian Fault beneath the Marmara Sea, Turkey, deduced from long‐term ocean bottom seismographic observations. Issue 3 (6th March 2017)

• Record Type: Journal Article
• Authors: Yamamoto, Y.; Takahashi, N.; Pinar, A.; Kalafat, D.; Citak, S.; Comoglu, M.; Polat, R.; Kaneda, Y.
• Is Part Of: Journal of geophysical research. Volume 122:Issue 3(2017)
• Page Start: 2069
• Page End: 2084
• Publication Date: 2017-03-06
• Subjects: the North Anatolian Fault -- Marmara Sea -- seismicity -- fault geometry -- ocean bottom seismographic observation; Geomagnetism -- Periodicals; Geochemistry -- Periodicals; Geophysics -- Periodicals; Earth sciences -- Periodicals; 551.1
• DOI: 10.1002/2016JB013608
• Languages: English
• ISSNs: 2169-9313

Abstract

Abstract: Both the geometry and the depth of the seismogenic zone of the North Anatolian Fault under the Marmara Sea (the Main Marmara Fault (MMF)) are poorly understood, in part because of the fault's undersea location. We recorded 10 months of microseismic data with a dense array of ocean bottom seismographs and then applied double‐difference relocation and 3‐D tomographic modeling to obtain precise hypocenters on the MMF beneath the central and western Marmara Sea. The hypocenters show distinct lateral changes along the MMF: (1) both the upper and lower crust beneath the Western High are seismically active and the maximum focal depth reaches 26 km; (2) seismic events are confined to the upper crust beneath the region extending from the eastern part of the Central Basin to the Kumburgaz Basin; and (3) the magnitude and direction of dip of the main fault change under the Central Basin, where there is also an abrupt change in the depth of the lower limit of the seismogenic zone. We attribute this change to a segment boundary of the MMF. Our data show that the upper limit of the seismogenic zone corresponds to sedimentary basement. We also identified several seismically inactive regions within the upper crust along the MMF; their spatial extent beneath the Kumburgaz Basin is greater than beneath the Western High. From the comparison with seafloor extensometer data, we consider that these regions might indicate zones of strong coupling that are accumulating stress for release during future large earthquakes. Key Points: Long‐term ocean bottom seismic data identified a segment boundary of the Main Marmara Fault beneath the central basin of the Marmara Sea The seismogenic zone of the Main Marmara Fault locates beneath the sedimentary basement Zones of no seismicity within the upper crust appear to indicate locked sections of the Main Marmara Fault