Difference between revisions of "Dictionary:Seismic trace/es"

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{{Infobox dictionary  
{{Infobox dictionary  
  | term    = seismic trace
  | term    = seismic trace

Revision as of 13:56, 13 April 2019

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In seismology, a seismic trace refers to the recorded curve from a single seismograph when measuring ground movement. The name comes from the curve plotted by a seismograph as the paper roll rotated and the needle left a trace from which information about the subsurface could be extracted. Today's instruments record the data digitally and the word trace has come to mean the digital curve.

A regular set of measurements from one seismic channel (or stacked channels); a digital one-dimensional array of regularly sampled numerical values.

Complex seismic trace

The recorded seismic trace is considered the real part of the complex trace. By phase shifting the recorded trace by 90 degrees, we can obtain the imaginary part of the complex trace. The complex seismic trace is a complex function whose real and imaginary part are the previously mentioned.[1] From the complex trace, one can now define seismic attributes such as the complex amplitude, phase, instantaneous phase and instantaneous frequency.


  1. Barnes, A.E. (2007). "A tutorial on complex seismic trace analysis". Geophysics 72: W33-W43. doi:10.1190/1.2785048.