Pre-Geophysical Investigations of Golbasi Soils After February 6th 2023 Kahramanmaras Earthquakes


Özdağ Ö. C., Tatar O., Yerli B., Bulgurcu A., Özden G., Sözbilir H., ...Daha Fazla

Seismological Society of America (SSA) Annual Meeting 2023, San Juan, Porto Riko, 17 - 21 Nisan 2023, ss.1

  • Yayın Türü: Bildiri / Özet Bildiri
  • Basıldığı Şehir: San Juan
  • Basıldığı Ülke: Porto Riko
  • Sayfa Sayıları: ss.1
  • Dokuz Eylül Üniversitesi Adresli: Evet

Özet

On February 6th, 2023, earthquakes with magnitudes of 7.7 and 7.6 on the Richter scale

occurred in Pazarcik/Kahramanmaras and Elbistan/Kahramanmaras/Turkey, respectively, with

depths of 9 km and 7 km and at UTC times of 01:17 and 11:24. These earthquakes caused

significant loss of life and property in Eastern Turkey and Northern Syria. The district of Golbasi

in the province of Adiyaman was one of the areas highly affected by the earthquakes due to

both the bearing capacity loss of the soil and the location of the Pazarcik Segment of the

Eastern Anatolian Fault Zone passing through the district center. Two days after the

earthquake, the earthquake research and application center team from Dokuz Eylul University

conducted preliminary field observations in the region. Structural damage in Golbasi was

observed to be the result of soil-bearing capacity losses and possible liquefaction. It is known

that the ground in Golbasi is composed of ancient lake sediments. It is considered that site

soils in the region has caused significant soil amplification if they are highly plastic whereas

large deformations and dependent attenuation took place in low plastic clays with silt.

Therefore, it is essential to determine shear-wave velocity distribution as part of this study,

microtremor measurements were taken at a total of 32 points with a 300 m sampling interval

in the Golbasi district to establish an initial database that could be easily extended by further

measurements to be made in intermediate locations. As a result of the microtremor

measurements, the predominant vibration period of the region, the Kg damage index

parameter, and the shear wave velocity models in 1, 2, and 3 dimensions via a forward and

inverse solution of the HVSR curves were calculated, and presented.