Skip to content
Journal article

Late Quaternary sea-level highstands in the Tasman Sea: evidence from Lord Howe Island

Woodroffe C, Heijnis H, Price D, Murray-Wallace C, Bryant E, Brooke B ...see all

Marine Geology, vol. 125, issue 1-2 (1995) pp. 61-72

  • 1

    Readers

    Mendeley users who have this article in their library.
  • N/A

    Citations

    Citations of this article.
  • N/A

    Views

    ScienceDirect users who have downloaded this article.
Sign in to save reference

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

  • Coasts, reefs and atolls -- 76.4.3
  • Geographic: Tasman Sea -- 1-2 (61-72)
  • Sea level -- 71.3.8
  • The Holocene -- 72.7.7
  • coral reef

Get free article suggestions today

Mendeley saves you time finding and organizing research

Sign up here
Already have an account ?Sign in

Find this document

  • PMID: 1134484

Authors

  • C D Woodroffe

  • H Heijnis

  • D M Price

  • C V Murray-Wallace

  • E A Bryant

  • B Brooke

Cite this document

Choose a citation style from the tabs below