Abstract
In this study an attempt has been made to monitor and perform analysis to the occurred
earthquakes recorded by the installed seismometers in the close proximity to the Dokan
dam. Three-component continuous high resolution data logger seismometers had recorded
thousands of seismic events from January to December 2013. Twenty five earthquakes were
utilized for further processings that covered the studied area and surroundings. The
analyses include identifying the body waves from different azimuths within optimal range
of frequencies from 3 to 500Hz. The waveforms were used in determining the various
source parameters including location, focal depth and magnitude from their arrival times
and amplitudes. Epicentral map was drawn which depicts the epicentral distances of the
events from the source. Furthermore, the estimated crustal structure below the studied
area reveals that the seismic activities were occurred in shallow depths (less than 10 km)
within the upper part of the crust and the resulted average values for the P- and S-wave
velocities were 5.97 km/sec and 3.23km/sec respectively
earthquakes recorded by the installed seismometers in the close proximity to the Dokan
dam. Three-component continuous high resolution data logger seismometers had recorded
thousands of seismic events from January to December 2013. Twenty five earthquakes were
utilized for further processings that covered the studied area and surroundings. The
analyses include identifying the body waves from different azimuths within optimal range
of frequencies from 3 to 500Hz. The waveforms were used in determining the various
source parameters including location, focal depth and magnitude from their arrival times
and amplitudes. Epicentral map was drawn which depicts the epicentral distances of the
events from the source. Furthermore, the estimated crustal structure below the studied
area reveals that the seismic activities were occurred in shallow depths (less than 10 km)
within the upper part of the crust and the resulted average values for the P- and S-wave
velocities were 5.97 km/sec and 3.23km/sec respectively
Keywords
crustal structure
event waveform
magnitude
seismic signal
Abstract
تم إجراءرصد و تحليل الزلازل المسجلة بجهازالسايزموميتر المثبت بالقرب من سد دوكان في هذه الدراسة. سجلت الالاف من الهزات بدقة و باستمرار و على ثلاثة محاور خلال الفترة الممتدة بين كانون الثاني الى كانون الاول2013. استخدم خمسة وعشرون زلزالا لمزيد من المعالجات وقد غطت المنطقة المدروسة والمناطق المحيطة بها.تم تحديد الموجات الجسمية للهزات والصادرة من اماكن مختلفة وبتردد( 3 -500 هرتز). واستخدمت الموجات لتحديداماكن ،عمق و مقدار الهزات من ازمنة وصول الموجات و سعتها. ورسمت خريطة لمواقع الهزات وبعدها عن المصدر.علاوة على ذلك تم ايجاد تركيب القشرة تحت منطقة الدراسة و يدل على أن الانشطة الزلزلية حدثت في أعماق ضحلة (أقل من 10 كم) داخل الجزء العلوي من القشرة. وان معدل قيم سرعة الموجات الأولية والثانوية هي 5.97 و3.23 كم /ثا على التوالي.
Keywords
شكل الموجة للحدث، المقدار، تركيب القشرة، االشارة زلسالية.