1973
DOI: 10.1038/physci245109a0
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Gambier-Beaconsfield and Gambier-Sorell Fracture Zones and the Movement of Plates in the Australia-Antarctica-New Zealand Region

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Cited by 30 publications
(10 citation statements)
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“…These amalgamated terranes are thought to have been 200-300km closer to the Adelaide region of South Australia than they are now, in Early to Middle Devonian time, due to net sinistral movement along the Gambier-Tamar Fracture Zone (Harrington et al 1973;Williams 1978). If these beliefs are correct, the original latitude of the Point Hibbs Limestone and its important Pragian coral fauna, which are part of the Tyennan terrane, would have been about 42~ on the Scotese Emsian reconstruction.…”
Section: Eastern Australiamentioning
confidence: 98%
“…These amalgamated terranes are thought to have been 200-300km closer to the Adelaide region of South Australia than they are now, in Early to Middle Devonian time, due to net sinistral movement along the Gambier-Tamar Fracture Zone (Harrington et al 1973;Williams 1978). If these beliefs are correct, the original latitude of the Point Hibbs Limestone and its important Pragian coral fauna, which are part of the Tyennan terrane, would have been about 42~ on the Scotese Emsian reconstruction.…”
Section: Eastern Australiamentioning
confidence: 98%
“…For instance, many interpretations conclude by requiring that Tasmania shifts some hundreds of km along an eastwest, either sinistral or dextral Palaeozoic strike-slip fault in Bass Strait (Harrington et al, 1973;Baillie, 1985;Stump et al, 1986;Elliott and Gray, 1992;Betts et al, 2002), often referred to as the Colac-Rosedale Fault. However, there is a lack of evidence for the existence of this fault from available data (e.g., modern magnetic and gravity datasets do not show evidence for any lateral offset between Tasmania and Victoria), including no persuasive along-strike correlation in terms of stratigraphy and metamorphic history.…”
Section: Introductionmentioning
confidence: 98%
“…These rocks are evidence of volcanic activity in the early stages of the rift. Jurassic dolerites of Antarctica and Tasmania (discussed by Harrington et al, 1973) may also be associated with the rifting. Falvey (1974) has concluded that the Lower Cretaceous non-marine Otway Group sediments in the Otway Basin are a relic of a prerift intracratonic basin and that the unconformity between the Upper Cretaceous marine Sherbrook Group and the Otway Group marks the onset of rift formation.…”
Section: Features Related To the Rifting Of Australia And A Ntarcticamentioning
confidence: 96%