1 / 7

Velsect Automatic Velocity Analysis

Velsect Automatic Velocity Analysis. General approach. Digitise sea floor and “base” events Where there is no data – or no moveout Create a rough water-depth based velocity field Create water-depth based NMO stretch mutes Filter data : tight band-pass and RADON

cmclemore
Download Presentation

Velsect Automatic Velocity Analysis

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Velsect Automatic Velocity Analysis

  2. General approach • Digitise sea floor and “base” events • Where there is no data – or no moveout • Create a rough water-depth based velocity field • Create water-depth based NMO stretch mutes • Filter data : tight band-pass and RADON • Generate velocity spectra and pick • Edit based on geological values • Extract low-spatial frequency component

  3. Avoiding Misspicks • Cycle skipping – different parts of same event • Band pass filter AND limit picking increment • Distorted semblance – multiples/diffractions • RADON filtering in “signal out” mode • High or low velocity trends • Reject picks on interval velocity – iteratively • Dip effects • Pick iteratively; stacks and preSTM data • Mispicks deleted prior to extracting trend

  4. Raw VELSECT picks Base horizon location can be easily identified Velocity trends are already clearly visible at this stage

  5. Edited VELSECT picks V-T pairs that give rise to interval velocities outside the range 1520m/s and 6000m/s rejected, iteratively. Aorund 30% of all V-T pairs rejected

  6. Final VELSECT picks 1.5km radius low-pass spatial frequency filter used to extract trend and remove jitter

  7. Final VELSECT results Water depth based velocities (left) and VELSECT velocities (right); note that dip and multiple are still present and this represents a first pass velocity field only

More Related