Cenozoic deformation in the Otway Basin, southern Australian margin: implications for the origin and nature of post-breakup compression at rifted margins

There is growing recognition that pulses of compressive tectonic structuring punctuate the post‐breakup subsidence histories of many ‘passive’ rifted continental margins. To obtain new insights into the nature and origin of compression at passive margins, we have conducted a comprehensive analysis of the post‐breakup (