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Seismic Velocity Models of the Sediments and Upper Crust of the Capel and Faust Basins, Lord Howe Rise

Created 20/01/2026

Updated 20/01/2026

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This report is a description of velocity data acquired during the summer of 2006/07 on Geoscience Australia's seismic marine reflection, refraction and potential field survey GA302 over the Capel and Faust Basins, Lord Howe Rise.

The survey was the final phase of the Australian Government's Big New Oil initiative commenced in 2003 to support acreage release in frontier basins. Previous data over the region are sparsely located, and the present survey will provide explorers with high quality data acquired and processed to modern standards.

The Lord Howe Rise is thought to be a continental fragment detached from Australia during the formation of the Tasman Sea. The Capel and Faust Basins are of interest as possible frontier petroleum provinces, and the present work is aimed at improving the confidence of sediment thickness estimation, a critical parameter in evaluating of prospectivity.

The study reviews the seismic reflection data from survey GA302, the sonobuoy refraction data acquired, and the stacking velocities from the seismic reflection processing.

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Title Seismic Velocity Models of the Sediments and Upper Crust of the Capel and Faust Basins, Lord Howe Rise
Language eng
Licence Not Specified
Landing Page https://data.gov.au/data/dataset/ba8dc25b-6cfe-4bce-a322-078cdc2a441c
Contact Point
Geoscience Australia Data
clientservices@ga.gov.au
Reference Period 20/04/2018
Geospatial Coverage
Map data © OpenStreetMap contributors
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Data Portal Data.gov.au