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- W2792277897 abstract "ABSTRACTThe coarse-grained, upper Cambrian Owen Group of western and northern Tasmania is a prominent feature of the Tasmanian landscape and regional map series. The group has previously been divided into four informal formations (Lower Owen Conglomerate, Middle Owen Sandstone, Middle Owen Conglomerate and Upper Owen Sandstone) that have been correlated across the state over tens to hundreds of kilometres. The deposition of these sediments is largely believed to have occurred during extensional tectonics, but some authors continue to argue a compressional tectonic regime. Detailed mapping and sedimentological work around Proprietary Peak on the Mount Jukes massif, 10 km south of Queenstown, Tasmania, has identified significant depositional variations controlled by early growth faulting and paleotopography. Discontinuity of stratigraphic units (L6–L13) across two growth faults on the north face of Proprietary Peak shows the strong effect on sediment deposition in the area. Paleotopography is also evident w..." @default.
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- W2792277897 date "2018-01-28" @default.
- W2792277897 modified "2023-09-27" @default.
- W2792277897 title "Early growth fault activity: new evidence for extension in the upper Cambrian Owen Group, Proprietary Peak, western Tasmania, Australia" @default.
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- W2792277897 doi "https://doi.org/10.1080/08120099.2018.1413010" @default.
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