Abstract
Effective seismic interpretation requires correlating seismic data with well data. This is usually accomplished by visually correlating a synthetic seismogram, generated from sonic and density logs, with nearby seismic data. If a sonic log is not available but a density log is, then Gardner’s relationship is generally used to estimate sonic data. For those situations where synthetic seismograms are derived but sonic or density log data are not available, techniques have evolved to estimate the sonic traveltime from other well log data, primarily the resistivity curve.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
