The procedure to create a synthetic seismogram is as follows:
- Multiply the velocity (calculated from the sonic log) and density logs to generate an acoustic impedance (AI) log. When a density log is not available, the densities can be calculated from the velocities with Gardner's rule: the density is proportional to the ¼ power of the P-wave velocity. - Calculate from the AI log the reflection coefficients (using Zoeppritz' equation)- Determine the wavelet from the seismic data -Convolve the wavelet with the reflection coefficient trace to generate the synthetic trace
"Shake, Rattle, and Roll". But seriously folks, it's called a "seismogram".
seismogram
The trace produced by a seismograph is called a seismogram.
seismogram are the records or paper copies that are produced by seismographs used to calculate the location and magnitude of an earthquack
A seismogram is a record of an earthquake that's obtained from a seismic instrument. It's in the form of a graph.
Seismogram is a proper noun.When you type Seismogram you capitilize the S.
seismogram
Tsunamis
Most of vibrations can be detected and recorded by sensitive instruments called seismograph, or seismometers. The record produced by a seismometer is called a seismogram.
"Shake, Rattle, and Roll". But seriously folks, it's called a "seismogram".
The three waves that are shown on a seismogram in order are P waves, S waves, and surface waves.
The highest amplitudes on a seismogram are typically associated with the strongest seismic waves, such as surface waves. These waves have the most energy and cause the largest vibrations in the ground, resulting in the highest amplitudes recorded on the seismogram.
epicenter
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seismogram and seismograph!
the entisety of an earthquake
From one seismogram, you can learn about the timing, magnitude, and location of an earthquake. By analyzing the wave patterns captured on the seismogram, seismologists can determine the earthquake's Richter magnitude, depth, and distance from the seismograph station that recorded it.