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CRUSTAL THICK NESS AND BASEMENT DEPTH MAPPING USING INTEGRATED GRAVITY AND MAGNETICSURVEYSANDGEOLOGICALSAMPLING ALONG GAY ALTHAKOT SECTION OFTHE KARAK.ORAMHIGHWAY198687.A thesis submitted to the QUAIDIAZAMUNIVERSITY,ISLAMABADFOR
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01
Gather the geological and seismic data for the area of interest.
02
Identify the relevant frequencies and wavelength ranges for the seismic waves being analyzed.
03
Select the appropriate models for crustal structure based on existing literature or empirical data.
04
Calculate the intrinsic attenuation coefficient using laboratory measurements or empirical relationships.
05
Consider the effects of scattering and geometrical spreading on seismic wave propagation.
06
Combine the intrinsic attenuation with scattering effects to obtain the total crustal seismic attenuation.
07
Review and validate the results with field observations or other empirical data.

Who needs crustal seismic attenuation of?

01
Seismologists conducting research on seismic wave propagation.
02
Engineers designing structures in seismic-prone areas.
03
Geologists studying the Earth's crust and its properties.
04
Disaster management agencies planning for earthquake response.
05
Researchers involved in earthquake risk assessment and mitigation.
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Crustal seismic attenuation refers to the reduction of seismic wave amplitude as it travels through the Earth's crust due to scattering and absorption of energy.
Geophysicists, seismologists, and organizations involved in seismic studies or construction projects in seismically active areas are typically required to file crustal seismic attenuation reports.
To fill out a crustal seismic attenuation report, one must gather relevant seismic data, analyze it to determine attenuation characteristics, and complete the reporting form with the findings and methodologies used.
The purpose of crustal seismic attenuation reports is to assess seismic hazard levels, inform building codes, and enhance our understanding of earthquake effects in specific regions.
The report must include data on seismic wave propagation, attenuation coefficients, analysis methods, relevant geological conditions, and any supporting graphics or charts.
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