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Suspended-sediment transport and water movement at One Tree Reef, southern...
One Tree Reef, in the southern Great Barrier Reef, is roughly triangular, with the southeast corner forming the windward margin, and the northwest side the leeward margin. In... -
Application of entropy-ratio maps to surficial reef facies, Great Barrier Reef
Entropy-ratio maps enable mapping of surficial facies of coral reefs at any chosen resolution. A ternary classification uses detritus, framework encrustation, and pavement as... -
Thick ferromanganese deposits from the Dampier Ridge and the Lord Howe Rise...
Chemical and mineralogical data are presented for four ferromanganese samples (two nodules and two crusts) from two stations of the West German vessel Sonne. Three samples came... -
Structure and stratigraphy of the central Great Barrier Reef
The Cainozoic evolution of the central Great Barrier Reef Province has been deduced from shallow, intermediate, and deep focus seismic reflection profiling. For much of its... -
Pleistocene to Holocene planktic foraminiferal biostratigraphy of the Coral...
Fifteen of 27 potential planktic foraminiferal biostratigraphic events from the latest Pliocene-Holocene have been examined; most of the early Pleistocene was not able to be... -
Lord Howe Rise, Tasman Sea - preliminary geophysical results and petroleum prospects
The Lord Howe Rise is a major submarine feature in the Tasman Sea; it extends northwest from the New Zealand continental margin and lies about 600 to 1200 km off the east coast... -
Terrigenous sedimentation in the central Great Barrier Reef lagoon: a model...
The central Great Barrier Reef Province is characterised by a mainland prograding terrigenous clastic shoreline and an inner shelf dominated by fluvially derived mud. The... -
Some aspects of lagoon sedimentation and circulation at One Tree Reef,...
Observations of water movement at One Tree Reef under modal wind, wave, and tide conditions show that the lagoon currents are insufficient to entrain lagoon sediments and cannot... -
Epeiric carbonate sedimentation of the Ninmaroo Formation (Upper...
The Ninmaroo Formation (Upper Cambrian-Lower Ordovician) is one of several epeiric carbonate sequences in the Georgina Basin. It comprises ooid, peloid, flat-pebble... -
Great Artesian Basin - Geomorphology
This dataset classifies the geomorphological features of the GAB and includes the offshore extents of the GAB beneath the Gulf of Carpentaria. The geomorphological... -
The Great Artesian Basin, Australia
The Great Artesian Basin occupies 1.7 X 10^6 km^2, or about one-fifth of Australia, extending across parts of Queensland, New South Wales, South Australia, and the Northern... -
Holocene Palaeo-Environmental changes, central to north Great Barrier Reef inner zone
Fringing reefs and storm ridges, from inner-shelf sites on the Great Barrier Reef between 14° and 20° S, are examined for Holocene sea-level and climatic changes. The sites... -
Global sea-level change as a method of correlating the Late Permian coal...
Eustatic changes in sea level can be used to correlate sequences in widely separated areas. Thick terrestrial sequences with marine intercalations are especially suitable,... -
Marine benthic communities in the Early Carboniferous of New South Wales...
The Delepinea aspinosa brachiopod Zone comprises two subzones: the Inflatia elegans and Linoprotonia tenuirugosa Subzones. Multivariate (cluster) analysis is used to identify... -
Lithology and diagenesis of the carbonate foundations of modern reefs in the...
In the southern Great Barrier Reef a relativel y thin (< 20 m) Holocene reef has developed on a foundation comprising a succession of older reefs. This reef foundation... -
Seismic refraction - a tool for studying coral reef growth
Seismic refraction studies have been conducted in close proximity to shallow boreholes previously drilled at Bewick (Northern Great Barrier Reef), Hayman (Central Great Barrier... -
Late quaternary regional controls on the development of the Great Barrier...
High-resolution seismic reflection data have been examined in an attempt to identify and explain some of the regional differences and controls on the development of the Great... -
Sedimentary cycles in the Surat Basin and global changes of sea level
Six sedimentary cycles, each hundreds of metres thick, have been recognised in the Surat Basin. The Jurassic cycles (nos. 1-4) typically started with high-energy deposition of... -
Drowned dolines - the blue holes of the Pompey Reefs, Great Barrier Reef
Blue holes occur at Cockatoo and Molar Reefs, in the Pompey hard line reefs. These two holes are roughly circular in shape, between 240-295 m in diameter, and 30-40 m deep. They... -
Numerical techniques applied to the geochemistry of some estuarine sediments...
Q-mode factor analysis classified the estuarine samples from Broad Sound into two main geologically distinct groups representing intertidal and supratidal deposition. This...