Fifteen non-palinspastic palaeotectonic maps, and accompanying explanatory text, are
presented to illustrate the progressive development of the Australian continental block from …

11. Seismic structure section across the subduction system of the Java Trench Sections
through the subduction system of southern Sumatra...... 12. Age determinations of granitic …

The continental crust is exposed in cross-section at numerous sites on the earth's surface.
These exposures, which appear to have formed by obduction along great faults during …

Three main basement provinces can be recognized in Australia, viz. Tasman (Late
Precambrian-Phanerozoic), Arunta-Gawler (Early and Middle Proterozoic), Pilbara-Yilgarn …

The locus of intraplate deformation in central Australia changed from the presently
preserved southern margin of the Amadeus Basin during the late Neoproterozoic to early …

Abstract The Geological Survey of Norway (NGU) has produced new aeromagnetic and
gravity maps from Norway and adjacent areas, compiled from ground, airborne and satellite …

Southwestern Australia has a long dynamic Precambrian history of crustal fragmentation
and aggregation by continental collision and accretion. This interpretation contrasts with the …

Until now, there has been no clear evidence from deep seismic reflection profiles of crustal
faults that displace the Moho. New data from central Australia show such a structure in a …

The intracratonic Amadeus Basin in central Australia is a complex, composite basin covering
17,000 km², with at least nine distinct episodes of evolution between 900 and 300 Ma. These …

The central Australian geology is dominated by a series of parallel sedimentary intracratonic
basins whose history spans time from the Late Proterozoic to the Carboniferous. The basins …