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Styles of neotectonic fault reactivation within a formerly extended continental margin, North West Shelf, Australia
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New evidence for neotectonic deformation in tectonically stable western Australia.

Transcurrent reactivation evident in a large-scale restraining bend within the WASZ.

Styles of reactivation show interaction of relic structures and modern stress field.

The western margin of Australia does not meet the definitions of a SCR.

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