Seismic attenuation in the Delaware Basin

  • M. Drwila*
  • , L. Eisner
  • , Z. Jechumtálová
  • , D. Anikiev
  • *Corresponding author for this work

Research output: Chapter in Book/Report/Conference proceedingConference contributionpeer-review

Abstract

Induced seismicity in Delaware Basin (West Texas and New Mexico, USA) has recently gained attention of the geoscience community. The knowledge about seismic attenuation in this sedimentary basin is poor. The peak frequency method was applied to the selected seismic events with high signal-to-noise ratio from the Delaware Basin to estimate effective quality factors of the basin sediments. The observed attenuation can be characterized by Q factors of approximately 90 and 100 (with uncertainty of 30) for P-wave and S-waves, respectively. The ratio between Qp and Qs is common for saturated sedimentary basins as they are less attenuating the S-waves.

Original languageEnglish
Title of host publication7th EAGE Workshop on Passive Seismic 2018
PublisherEuropean Association of Geoscientists and Engineers, EAGE
ISBN (Electronic)9789462822443
StatePublished - 2018

Publication series

Name7th EAGE Workshop on Passive Seismic 2018
Volume2018-March

Bibliographical note

Publisher Copyright:
© 2018 European Association of Geoscientists and Engineers EAGE. All rights reserved.

ASJC Scopus subject areas

  • Geotechnical Engineering and Engineering Geology
  • Geophysics

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