Example of the H–K and depth stacking analysis for the station LOD (39.89〈°〉N, 32.76〈°〉E).
The majority of stations with either the backazimuth variation of the Ps or a high ratio are located either along the western and southern coastlines or within the Eastern Anatolian Plateau (See supplemental data table). 3(a) shows four layers between depths of 3 and 29 km, the velocity being 6.25 km s−1 at depths between 15 and 21 km.
1a) in the African-European convergent tectonic setting has resulted in a complex deformation history with several large-scale tectonic features.
The located events do not follow mapped faults in the area. 2 shows an example of the typical receiver functions both radial and transverse, labelled R and T respectively, generated by the process described above for the Kandilli array station LOD (39.89°N, 32.76°E).
Three different velocity models were used as initial models for the inversion: The first is a model obtained by finer sampling of the model which is routinely used by KOERI (Table 1), the second is generated by using available geological information on the crustal structure and the last is a velocity model with constant velocity. Figure S3. Nihal Akyol, Lupei Zhu, Brian J. Mitchell, Hasan Sözbilir, Kıvanç Kekovalı, Crustal structure and local seismicity in western Anatolia, Geophysical Journal International, Volume 166, Issue 3, September 2006, Pages 1259–1269, https://doi.org/10.1111/j.1365-246X.2006.03053.x.
Effects on receiver functions and a case study in New Zealand, Variations in the crustal structure benath Western Turkey. (1998) have been included in the mapping process. The large deviations indicate of significant lateral variation in crustal velocity structure. Magnesium : 915 mg 30.5
Husen S.
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Ray coverage of 245 events located by VELEST (Kissling 1994). Turkish figs are just dried in the sun at Aydin and Izmir provinces. We obtained a 1-D P-wave crustal velocity model using a generalized scheme for simultaneously obtaining earthquake locations and a crustal velocity model. 2) also yielded station corrections (Fig. The upper right panels are the two H–K stacks with a weighting of 0.5 on the Ps and 0.5 on the 2p1s (labelled 100/0) or a weighting of 0.5 on the Ps, 0.25 on the 2p1s, and 0.25 on the 1p2s phases (labelled 50/50). Two distinct Neogene deformation phases dominated by strike-slip faulting. For full access to this pdf, sign in to an existing account, or purchase an annual subscription. We then used VELEST (Kissling 1994) inversion algorithm, to solve for hypocentral locations, the minimum 1-D velocity model, and associated station delays using only P-wave arrivals for all selected events. Şengör (1985) suggested that the crust in western Anatolia had thickened to about 50 to 55 km by Early Miocene time as a result of Palaeocene orogenic contraction. 8b). The current extension oriented approximately N–S is occurring at a rate of 30–40 mm yr −1 (McKenzie 1978; Taymaz 1991) in the region, and has replaced the Palaeocene orogenic contraction (e.g. Tectonics and Magmatism in Turkey and the Surrounding Area, Crustal Thickness Variation in the Aegean Region and Its Implications for the Extension of Continental Crust, Seismotectonics of Western Turkey from high resolution earthquake relocations and moment tensor determination, © 2006 The Authors Journal compilation © 2006 RAS, Scalar magnetic difference inversion applied to UAV-based UXO detection, On-axis triplications in elastic orthorhombic media, Pseudo-probabilistic identification of fracture network in seismic clouds driven by source parameters, The effects of Earth model uncertainty on the inversion of seismic data for seismic source functions, Volume 223, Issue 2, November 2020 (In Progress), Volume 223, Issue 3, 1 December 2020 (In Progress), Geomagnetism, Rock Magnetism and Palaeomagnetism, Marine Geosciences and Applied Geophysics, https://doi.org/10.1111/j.1365-246X.2006.03053.x, Receive exclusive offers and updates from Oxford Academic, Copyright © 2020 The Royal Astronomical Society.
Kissling E.
The most distinct large scales feature of the Anatolian Plate is the gradient from a thinner crust in the extensional West to a ‘normal’ crustal thickness in central Anatolia to a thickened crust in the compressional regime in eastern Anatolia (Fig. and they were spread through the Mediterranean from Anatolia …
Aldanmaz 2002; Tonarini 2005).
2. The kinematics and evolution of the southern part of the İBTZ are well constrained, but its northern continuation remains unstudied. In fact, the first successful harvest of Smyrna figs in California was 1900.
2.
Caria became subject to Persia, Greece and Rome before being absorbed into Byzantium. We also thank Michelle Salmon for her useful advice in generating the large-scale maps. We further mask the portions of the resulting surface that are further than 75 km away from individual station locations to avoid attributing either a Moho depth or VP/Vs ratio to an undersampled portion of the overall plate. Note that in this particular case the H–K stack and depth stack determination of Moho depths are in good agreement because the VP/Vs ratio determined by the H–K method is close to the 1.73 VP/Vs ratio of the IASP91 model (Kennett & Engdahl 1991).
Due to inadequate azimuthal and take-off angle distributions, the depth values were constrained for C-class events. Kendall J.-M. Baer M. Phone: +90 (232) 799 0292 (pbx) Fax: +90 (232) 799 0113, Factory and Head Office Address:
As water at the outer level of dried figs evaporate, natural sugars crystallize on the outer surface of dried figs.
Data from the regional array instruments, plus selected data from the linear array stations were used to locate local events.
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