Australian jurassic sedimentary and fossil successions: Current work and future prospects for marine and non-marine correlation

Susan Turner*, Lynne B. Bean, Mary Dettmann, John L. McKellar, Stephen McLoughlin, Tony Thulborn

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

93 Citations (Scopus)

Abstract

Strata of Jurassic age occur extensively across onshore Australia, but they are predominantly of non-marine origin. Marine Jurassic strata have only limited onshore exposure in northwestern and central-western Australia, with thick marine sequences lying offshore on the North West Shelf. The richest petroleum province in Australia is located at the shelf's southern end, where the Dingo Claystone represents an important source rock for oil and gas. By and large, non-marine deposits, including economic coals, are distributed in the eastern states. Jurassic stage boundaries, in the main, are poorly constrained with respect to the Australian sedimentary succession. New work on microfossils, plants, fish, and zircon dating is providing a basis for improved correlation across Australian basins, with overseas successions, and recent international IUGS geologic timescales.

Original languageEnglish
Pages (from-to)49-70
Number of pages22
JournalGFF
Volume131
Issue number1-2
DOIs
Publication statusPublished - Jun 2009

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