Sigsbee2B FS & NFS 2D Synthetic Datasets

October 2002

The Subsalt Multiples Attenuation and Reduction Technology Joint Venture (SMAART JV) is releasing to the industry and universities the 2D acoustic synthetic datasets referred to as Sigsbee2B FS and Sigsbee2B NFS. The Sigsbee2B dataset is featured in paper SP3.8 "Observations from the Sigsbee2B synthetic dataset" at the 2002 SEG meeting in Salt Lake City. The current release includes the velocity model and allows anyone to use the data and to publish the results under the conditions described in the Data Release Agreement.

Sigsbee2B models the geologic setting found in on the Sigsbee escarpment in the deep water Gulf of Mexico as shown in Sigsbee2B Stratigraphy. The model exhibits the illumination problems due to the complex salt shape with rugose salt top found in this area. The dataset was calculated with an absorbing free surface condition and a weaker than normal water bottom reflection, i.e. the data do not contain free surface multiples and less than normal internal multiples. The color scale in this stratigraphy plot is chosen to emphasize reflectors and faults and does not represent the real velocity contrasts. A number of normal and thrust faults separate the sedimentary blocks. The syncline segments of the salt top focus reflection energy from the salt bottom and the sub salt reflections and produce non-hyperbolic arrival travel time curves.

The stratigraphic velocity model is shown in Sigsbee2B Interval Velocity. The reflection interfaces are all the result of velocity contrasts, which are fluctuations about a mean velocity V + Vo + kZ. The relative velocity fluctuation average dV/V is about 0.03, which is enough to produce reflections, but not sufficient to destroy the basic gradient macro model Sigsbee2B Migration Velocity which is used in depth migration.

For more details on the construction and numeric computation of the dataset, see the Sigsbee2B Distribution file.

This release is available via the Smaart Data Administrator. Contact the Smaart Data Administrator for prices.

To obtain the data, sign the Data Release Agreement (PDF file) and mail it to Henry den Bok.

Delft University of Technology
Faculty of Applied Sciences
Acoustical Wavefield Imaging
attn. Henry den Bok
P.O. Box 5046
2600 GA Delft
The Netherlands.

To contact the Smaart Data Administrator, send email to Henry den Bok

We hope you will find the data useful for current and future research.

Henry den Bok
Smaart Data Administrator