Abstract
This mid-ocean island, which is the site of the southernmost coral reef, is composed of basalts of late Tertiary age, and calcarenites derived from bioclastic reefal carbonates. Both
Author supplied keywords
Cite
CITATION STYLE
APA
Woodroffe, C. D., Heijnis, H., Price, D. M., Murray-Wallace, C. V., Bryant, E. A., & Brooke, B. (1995). Late Quaternary sea-level highstands in the Tasman Sea: evidence from Lord Howe Island. Marine Geology, 125(1–2), 61–72.
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.
Already have an account? Sign in
Sign up for free