TY - JOUR
T1 - Seismic time reversal mirror experiment
AU - Landa, Evgeny
AU - Yurman, Adi
AU - Jenneskens, Rob
N1 - Publisher Copyright:
© 2019 EAGE Publishing BV. All rights reserved.
PY - 2019
Y1 - 2019
N2 - Time Reversal Mirror (TRM) is a method for refocusing recorded waves (including seismic) to their initial source location. Using different observation geometries, we demonstrate how seismic P- and S- energy is successfully focused back to its original location in a field experiment. Focusing resolution is within the theoretical range of half the dominant wavelength. Although the field experiment is done in controlled conditions, a-priori knowledge of seismic velocities of the medium is not necessary. In the first step the seismic wave is generated by a sub-surface point source and recorded by a surface array (the mirror). In the second step, time-reversed traces are back-propagated from the original receiver positions and recorded at locations near and at the original source location. The ability to carry out seismic TRM is dependent on a new vibrator based on a linear synchronous motor (LSM). As opposed to standard hydraulic-based seismic vibrators, the LSM-based vibrator can generate an arbitrary signal and thus re-emit recorded seismic traces back into the sub-surface. Various applications of the TRM in seismic data can be considered: enhance oil recovery by wave stimulation, fracking intensification, target oriented data acquisition etc.
AB - Time Reversal Mirror (TRM) is a method for refocusing recorded waves (including seismic) to their initial source location. Using different observation geometries, we demonstrate how seismic P- and S- energy is successfully focused back to its original location in a field experiment. Focusing resolution is within the theoretical range of half the dominant wavelength. Although the field experiment is done in controlled conditions, a-priori knowledge of seismic velocities of the medium is not necessary. In the first step the seismic wave is generated by a sub-surface point source and recorded by a surface array (the mirror). In the second step, time-reversed traces are back-propagated from the original receiver positions and recorded at locations near and at the original source location. The ability to carry out seismic TRM is dependent on a new vibrator based on a linear synchronous motor (LSM). As opposed to standard hydraulic-based seismic vibrators, the LSM-based vibrator can generate an arbitrary signal and thus re-emit recorded seismic traces back into the sub-surface. Various applications of the TRM in seismic data can be considered: enhance oil recovery by wave stimulation, fracking intensification, target oriented data acquisition etc.
UR - http://www.scopus.com/inward/record.url?scp=85072306770&partnerID=8YFLogxK
U2 - 10.3997/1365-2397.2019018
DO - 10.3997/1365-2397.2019018
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AN - SCOPUS:85072306770
SN - 0263-5046
VL - 37
SP - 41
EP - 45
JO - First Break
JF - First Break
IS - 6
ER -