The director of the earthquake in Khorasan Razavi Province’s Earthquake, Housing and Urban Development Center, said: It is estimated that segments of long and seismic faults stretched in the vicinity of the earthquake are the cause of this seismic event.
Dr. Ali Beitollahi in an interview with ISNA, Referring to the Geo Physics Institute report on the earthquake of Rashtkhvar Khorasan Razavi province, the earthquake was recorded at a depth of 2 kilometers and 2 km north of Rashtkhvar, 2 kilometers southeast of Dolatabad and 2 km southeast of Torbat Heydariyeh Khorasan Razavi province.
He said: For the earthquake of Rasht Khorasan Razavi province, based on empirical relations, the intensity of 2 miles and a radius of 1.5 kilometers around it, the severity of 2 to the radius of 1.5 kilometers and the severity of 2 to the radius of 1.5 km from the earthquake.
Beitullahi said that in the earthquake range of Rashtkhvar, 5 urban populations and 5 rural populations are resident, he continued: 2 cities are about 2 kilometers around the earthquake, the nearest cities include Rashtkhvar, Dolatabad, Torbat.
The director of the earthquake in the Road, Housing and Urban Development Center pointed to the fault of the earthquake. It extends more than 2 kilometers in the vicinity of the earthquake.
He emphasized: The rise of this fault may have caused the earthquake of Rasht Khorasan Razavi province.
Beitollahi pointed to the seismic history of Khorasan Razavi province and noted: According to modern Iran’s seismic data since the beginning of the year, and in the radius of one degree of earthquake -centricity, the earthquakes have been collected in the last 5 years that represent the seismic scope of the earthquake. Based on the data collected during this time.
He added: The number of earthquakes with a size of 4.3 and above has been recorded in the area around Roma from the age of 6 until the earthquake of Khorasan Razavi province (2 years). Of these, 2 earthquakes of 1 and above and 2 earthquakes with a size of 1 to 2 and the rest of the earthquakes are smaller than the size of the 2 -century.
According to him, the Kashmir earthquake, which is magnified on June 5, 2008, and the events of 1, 2.3 and 2.3 are among the recent and modern seismic events along this central Iran’s seismic fault.
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