-
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... -
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... -
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... -
The determination of suspended-sediment loads in the southern Great Barrier...
A mechanical system for collecting samples of suspended sediment in the water column at various stages of a tidal cycle, together with measurement of tidal current velocities,... -
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... -
Early Devonian thelodonts (Agnatha) from the Toko Syncline, western...
Thelodont scales recovered from the basal (calcareous) unit of the Cravens Peak Beds in the Georgina Basin, are referable to Turinia australiensis Gross, 1971, T. cf. pagei... -
Diagenesis of Jurassic and Lower Cretaceous sandstones of the Eromanga Basin...
The Jurassic and Lower Cretaceous sandstones of the Eromanga Basin in New South Wales can be divided into quartzose and volcanolithic petrofacies. The latter comprises... -
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... -
Miocene to Pleistocene foraminiferal biostratigraphy of dredge samples from...
Planktic and larger benthic foraminiferids have been studied in thin section from a suite of dredge samples of two sites on the Marion Plateau, offshore Queensland. The two... -
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... -
High-energy reef and terrigenous sedimentation, Boulder Reef, Great Barrier Reef
Sediment and water flux were monitored at Boulder Reef, in the Northern Great Barrier Reef, before, during, and after the passage of Tropical Cyclone Dominic. Rainfall at... -
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... -
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... -
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... -
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... -
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... -
Shallow inter-reefal structure of the Capricorn group, southern Great Barrier Reef
276 km of continuous seismic reflection profiles have been obtained from the inter-reef areas of the Capricorn Reefs. Five reflectors were identified, three being widespread:... -
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... -
The nature and origin of beach ridges, western Cape York Peninsula, Queensland
Two sets of beach ridges are known from the western side of Cape York Peninsula. The older set are thought to be late Pleistocene. They rest on a basement of older fan deposits...