Abstract
In areas of uniform lithology which have not undergone tectonic inversion or severe structural deformation, depth conversion can often be performed according to some simple mathematical function (e.g., average velocity as a linear function of depth). In areas where there are dramatic changes of velocity, such as thick carbonate or evaporite units alternating with thick clastic units (as those found in the southern North Sea basin), then simple functions cannot adequately cope with the inherent velocity inversions and are inadequate for depth conversion.
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.
