FULL WAVEFORM MODELLING FOR SUBSURFACE CHARACTERIZATION WITH CONVERTED-WAVE SEISMIC REFLECTION: COMPARISON OF P-P AND P-S FOR A THINBED SUBSURFACE
The ability of P-S converted-wave to image the complex geology structure is more reliable than the P-P. In the same P-wave frequency bandwidth, S-wave has the shorter wavelength, therefore the vertical resolution of the S-wave is higher than the P-wave. Using multicomponent receiver, the seismic...
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Format: | Final Project |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/44006 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | The ability of P-S converted-wave to image the complex geology structure is more
reliable than the P-P. In the same P-wave frequency bandwidth, S-wave has the
shorter wavelength, therefore the vertical resolution of the S-wave is higher than
the P-wave. Using multicomponent receiver, the seismic signals are recorded on
the vertical and horizontal components. Both of P-P and P-S wave are recorded on
these components, however due to their displacement vector the P-P data would be
dominated on the vertical component while on the horizontal component is
dominated by the P-S data. The aim for this study is to compare the behavior of the
P-P and P-S for the subsurface imaging especially for the existence of a thin-bed.
To achieve the purpose of this study, a synthetic model of a thin-bed underneath
gas layer was generated by the full waveform modelling. The P-P and P-S seismic
data processing are performed to obtain the seismic sections. Processing is also
carried out by extracting P-S wave from vertical component. Stack section does not
indicate any seismic event, that frequency and fresnel zone analysis of both P-P and
P-S waves are performed. The result of this study presents the resolution of P-S is
way more reliable than the P-P quality. However, extracting P-S wave from vertical
component is more difficult as lower dominant frequency and higher gamma
function. This depends on configuration and parameters of the seismic acquisition
geometry. |
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