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Determination of the Crust and Upper-Mantle Structure in Anatolia by Surface Wave Data

机译:利用表面波数据确定安纳托利亚地壳和上地幔结构

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In this study, the crust and upper mantle structure of Anatolia have been investigated by measuring the group velocity dispersion data of discriminated seismic surface waves. In the scope of the study, it has selected the profiles between six stations located in western Anatolia of Bogazici University Kandilli Observatory Earthquake Research Institute, national network of Turkey, and records of an earthquake (having about 10° epicentral distance) occurred in the eastern of Anatolia have been used. Firstly, surface wave discrimination filter based on the polarization properties has been applied tothree-component recordsand emphasized to surface waves. Then the group velocities have been calculated by multiple filter technique. A five-layered crustal model having total thickness of 38 - 40 km and Pn-wave velocity of 8.00 km/sec in the upper-mantle has been determined through inversion of surface wave group velocity dispersion data in the period range of 10 sec to 60 sec.
机译:在这项研究中,安纳托利亚的地壳和上地幔结构是通过测量已识别地震面波的群速度色散数据来研究的。在研究范围内,它选择了位于土耳其全国网络的博加兹奇大学坎迪利天文台地震研究所位于安纳托利亚西部的六个测站之间的剖面,并确定了东部地震发生的记录(震中中心距离约为10°)使用了Anatolia。首先,将基于偏振特性的表面波判别滤波器应用于三分量记录,并重点研究了表面波。然后通过多重滤波技术计算了群速度。通过在10 sec到60的周期范围内对面波群速度色散数据进行反演,确定了上地幔总厚度为38-40 km,Pn波速度为8.00 km / sec的五层地壳模型。秒

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