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New K-Ar constraints on the onset of subsidence in the Canning Basin,...
Structural mapping and reconnaissance K-Ar studies have helped to delineate and date the latest deformational stages (D4 and D5) in the King Leopold Orogen, to the north of the... -
Geochemical evaluation of the Petroleum Potential of the Toko Syncline,...
In the Georgina Basin, the Toko Syncline is considered the most prospective region for petroleum exploration. The syncline contains up to 5000 m of Middle Cambrian to Middle... -
Quaternary Antarctic ice-sheet fluctuations and Southern Ocean...
In its first three years, the Antarctic CRC s Natural Variability Program has focussed research effort on understanding changes in the extent of the East Antarctic ice sheet,... -
Surface-wave magnitudes of some early Australian earthquakes
Surface-wave magnitudes (Ms) of 35 of the larger Australian earthquakes that occurred before 1960 have been determined from seismograms written at Riverview (Sydney), Melbourne,... -
The crustal structure of the Gulf of Papua and northwest Coral Sea
Interpretation of seismic refraction data from the southwestern coast of the Papuan Peninsula and the northwest Coral Sea gives consistent results using several inversion... -
Australian national airborne geophysical databases
The Australian Geological Survey Organisation maintains national databases of aeromagnetic, radiometric and digital elevation data, which have been progressively collected since... -
Mode of emplacement of the Papuan Ultramafic Belt: a discussion
Connelly (1979) states: "Geological and geophysical evidence from a number of studies has established that the Papuan Ultramafic Belt is probably an overthrust sheet of oceanic... -
BMR journal of Australian geology and geophysics vol.1 no. 4
Contents: 1.Dooley JC, Barlow BC. Gravimetry in Australia, 1819-1976. 2.Anfiloff W, Barlow BC, Murray A, Denham D, Sandford R. Compilation and production of the 1976 1:5 000 000... -
The mineral potential of the Arunta Block, central Australia
The Arunta Block is the mass of Precambrian basement rocks in the southern part of the Northern Territory of Australia. It comprises an early Proterozoic (or older)... -
Evidence on the radius of the Precambrian Earth
It is suggested that the early and middle Proterozoic crustal record is inconsistent with, and cannot be explained on, an Earth of present-day dimensions (Glikson, in prep.).... -
Stratigraphic correlations in the Tennant Creek region, central Australia:...
The Proterozoic Warramunga Group, as previously mapped around Tennant Creek, is shown to consist of two sequences separated by a major angular unconformity. The older sequence,... -
Characterising the distribution of dissolved and residual NAPL petroleum...
In this paper, petroleum hydrocarbon contamination at two field sites is characterised extensively to provide data for risk assessment, and remediation design and monitoring. A... -
Upper Triassic spongiomorph and coral association dredged off the...
Upper Triassic corals and spongiomorphs dredged during BMR Cruise 95 from the Rowley Terrace, offshore Canning Basin of northwestern Australia, indicate possible new occurrences... -
A new local magnitude scale for southeastern Australia
Measurements of maximum trace amplitudes from 181 short- period vertical seismograms recorded at hypocentral distances of 3-1500 km from 36 earthquakes in the magnitude range... -
Stream-sediment sampling near two porphyry copper prospects, Georgetown...
The Phyllis May prospect is about 29 km west of Georgetown, north Queensland (Fig. 1). It was discovered in 1970 during geological prospecting by Central Coast Exploration NL,... -
Granitoids of northeastern Tasmania
The granitoids of northeastern Tasmania comprise the composite Scottsdale, Blue Tier, and Eddystone batholiths, and intrude the folded Ordovician to Lower Devonian Mathinna... -
Discussion: A review of the Corella Formation, Mount Isa Inlier, Queensland
Discussion is around the renaming of the Corella Formation (introduction of the name Doherty Formation), and potential down-grade of its status to beds. -
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... -
Forearc basin dynamics and sedimentation controls, Tamworth belt, eastern Australia
The eastern margin of the Australian continent was the site of convergent plate interaction for much of the Palaeozoic Era. The Tamworth Terrane, a forearc complex resulting...