The dense station spacing of DANA greatly aids in identifying and interpreting coherent reflections from subsurface interfaces beneath the array. We thank Andreas Fichtner and one anonymous reviewer for their insightful comments, which aided in the improvement of this manuscript.Please check your email for instructions on resetting your password.
Seismic imaging of active fault zones has provided two contrasting arguments: some authors, such as In contrast, other studies on continental strike slip faults [Here we aim to image the crustal structure of the North Anatolian Fault Zone (NAFZ) in Turkey in the region of the 1999 Izmit and Düzce earthquakes. The NAFZ formed in the middle Miocene and propagated westward to reach the Sea of Marmara ∼200 ka ago [In this region, the NAFZ divides into a northern and southern strand [Between May 2012 and October 2013, the University of Leeds, Kandilli Observatory and Earthquake Research Institute (KOERI) and Sakarya University installed a 66 station network of 3‐component seismometers in a roughly rectangular grid (Figure In order to image the structure of the NAFZ throughout the entire crust and upper mantle, we constructed stacked autocorrelograms of continuous seismic records from DANA.
The facilities of Bogazici University Kandilli Observatory and Earthquake Research Institute Data Services (KOERI DS) were used for access to waveform and metadata required in this study.
The earthquake ocurred where the North Anatolian Fault and the East Anatolian Fault meet. The KOERI DS is funded by the Ministry of Development of Turkey through the instrumentation and operation of the nationwide seismic network.
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The number of buildings damaged in the quake is not currently known, but there are reports of significant damage to mudbrick masonry structures and also to a small number of reinforced concrete structures.
Major funding was provided by the UK NERC under grant NE/I028017/1. The loss of coherence could be due to a loss of reflectivity but could also be due to the existence of small scale structure at the reflector. Our reflection profiles show a Moho reflected The behavior of fault zones within continental settings is more complex than simple plate tectonics would predict. White, upper crust; yellow, middle to lower crust; green, upper mantle; and brown, anisotropic upper mantle beneath Hales discontinuity. It has been proposed that ductile flow within the lower crust causes distributed deformation that otherwise occurs within narrow shear zones in the continental upper crust and upper mantle [In particular, understanding how structural changes throughout a fault zone can be used to infer the mechanism of strain localization at lower crustal depths has important implications for our knowledge of lithospheric rheology and our understanding of the earthquake cycle.
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North Anatolian Fault Map