The Australian-Antarctic sector of the Southern Ocean has been formed by asymmetric sea-floor spreading along an east-west trending ridge (Fig. 1). This ridge (the Southeast Indian Ridge) separates two major deep-water basins, the South Australian and South Indian Basins. Vigorous bottom-water circulation and regional productivity patterns have been important variables influencing sedimentation throughout the region.
CITATION STYLE
Williams, D. F., & Corliss, B. H. (1982). The South Australian Continental Margin and the Australian-Antarctic Sector of the Southern Ocean. In The Ocean Basins and Margins (pp. 545–584). Springer US. https://doi.org/10.1007/978-1-4615-8038-6_12
Mendeley helps you to discover research relevant for your work.