Abstract
Historically, geologic hazards have been primarily identified using high‐resolution 2-D single‐channel seismic (e.g., 3.5 kHz and minisparker records), side‐scan sonar surveys, geotechnical data from selected borings and in‐situ measurements, and drop cores. However, effective use of coherency and other seismic attributes on standard 3-D seismic data can allow early detection and delineation of both surface and subsurface geologic drilling hazards prior to the acquisition of high‐resolution “hazard” surveys.
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.
