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Investigation of 1-D Crustal Velocity Structure Beneath Izmir Gulf and Surroundings by Using Local Earthquakes

机译:用当地地震对伊兹密尔海湾和周围环境下的1-D地壳速度结构进行调查

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In this study; we examined one dimensional crustal velocity structure of Izmir gulf and surroundings. We used nearly one thousand high quality (A and B class) earthquake data which recorded by Disaster and Emergency Management Presidency (AFAD) [1], Bogazici University (BU-KOERI) [2] and National Observatory of Athens (NOA) [3,4]. We tried several synthetic tests to understand power of new velocity structure, and examined phase residuals, RMS values and shifting tests. After evaluating these tests; we decided one dimensional velocity structure and minimum 1-D P wave velocities, hypocentral parameter and earthquake locations from VELEST algorithm. Distribution of earthquakes was visibly improved by using new minimum velocity structure.
机译:在这项研究中;我们检查了Izmir海湾和周围环境的一维地带速度结构。我们使用了近一千个高质量的(A和B类)地震数据,由灾害和应急管理总统(AFAD)[1],Bogazici大学(Bu-Koeri)[2]和雅典国家天文台(NOA)[3 ,4]。我们尝试了几种合成测试以了解新速度结构的力量,并检查相残留,RMS值和转换测试。评估这些测试后;我们从Velest算法确定了一维速度结构和最小1-D P波速度,低速度参数和地震位置。使用新的最小速度结构明显地改善了地震的分布。

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