About Version 2
NCEI's global ocean sediment thickness grid (Divins, 2003) was updated for the Australian-Antarctic region (60°-155°E, 30°-70°S). Seismic reflection and refraction data were used to add detail to the conjugate Australian and Antarctic margins and intervening ocean floor where regional sediment thickness patterns were previously poorly known.
On the margins, sediment thickness estimates were computed from velocity-depth functions from sonobuoy/refraction velocity solutions ground-truthed against seismic reflection data. For the Southeast Indian Ridge abyssal plain, sediment thickness contours from Géli et al. (2007) were used.
The regional sediment thickness grid was combined with NCEI's original ocean sediment thickness grid (Divins, 2003) to create an updated global grid of ocean sediment thickness. Even using the minimum estimates, sediment accumulations on the extended Australian and Antarctic continental margins are 2km thicker across large regions and up to 9km thicker in the Ceduna Basin compared to NCEI's original sediment thickness grid (Divins, 2003), which has been deprecated but is still available.
Data Access
Citation
Géli, L., Cochran, J., Lee, T., Francheteau, J., Labails, C., Fouchet, C., and Christie, D., 2007, Thermal regime of the Southeast Indian Ridge between 88°E and 140°E: Remarks on the subsidence of the ridge flanks: J. Geophys. Res., v. 112, no. B10, p. B10101.
References
- Divins, D.L., Total Sediment Thickness of the World's Oceans & Marginal Seas, NOAA National Geophysical Data Center, Boulder, CO, 2003.
- Géli, L., Cochran, J., Lee, T., Francheteau, J., Labails, C., Fouchet, C., and Christie, D., 2007, Thermal regime of the Southeast Indian Ridge between 88°E and 140°E: Remarks on the subsidence of the ridge flanks: J. Geophys. Res., v. 112, no. B10, p. B10101.