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- W2122301182 endingPage "1598" @default.
- W2122301182 startingPage "1581" @default.
- W2122301182 abstract "This review synthesizes the Proterozoic and early Paleozoic geology of Tasmania, Bass Strait and western and central Victoria. We examine the many different conflicting hypotheses that have been proposed to solve the paradoxical relationships between Tasmanian geology and that of mainland Australia, most notably the prevalence of Proterozoic basement of western and central Tasmania, while immediately across Bass Strait evidence of Proterozoic rocks is much more cryptic. We conclude that the Selwyn block model is the most satisfactory hypothesis to date, since it fits best with the obvious patterns in the magnetic and gravity data. This model proposes that the central Victorian Melbourne Zone is underlain by the northern extension of thin Tasmanian Proterozoic and Cambrian crust under Bass Strait, and that the Silurian to Middle Devonian Melbourne Zone was shortened along a décollement during the Tabberabberan Orogeny. The Ordovician rocks of eastern Tasmania correlate more closely with the Tabberabbera Zone than the Melbourne Zone in Victoria; however the Silurian and Devonian correlations are less certain. Major unresolved issues are the origins of the Proterozoic and Early Cambrian lithostratigraphic packages, tectonic models for their assembly during the Tyennan Orogeny, and how these models fit with those for mainland Australia." @default.
- W2122301182 created "2016-06-24" @default.
- W2122301182 creator A5028528056 @default.
- W2122301182 creator A5045065273 @default.
- W2122301182 creator A5074885968 @default.
- W2122301182 date "2013-05-01" @default.
- W2122301182 modified "2023-10-06" @default.
- W2122301182 title "Towards understanding the early Gondwanan margin in southeastern Australia" @default.
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