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- W1488652023 abstract "Fault striations were measured on 104 minor faults within the Parmeener Super-group near Hobart. Thefault striations probably reflect the complex movement history on adjacent large faults. Sophisticated numericalmodelling of the regional stress systems which produced these striations indicated at least two phases of faulting. Theearlier phase was probably due to compression from the NNW in the Mesozoic and produced strike slip faults striking1000 and 1700C. The later phase of faulting was caused by extension towards the ENE in the Early to Middle Tertiary andreactivated most of the early phase faults striking 1700 , as normal dip slip faults. A small number of fault striationscould not be attributed to either of these events." @default.
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- W1488652023 date "1985-01-01" @default.
- W1488652023 modified "2023-09-24" @default.
- W1488652023 title "Striations on minor faults and the structure of the Parmeener Super-group near Hobart, Tasmania" @default.
- W1488652023 doi "https://doi.org/10.26749/rstpp.119.23" @default.
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