Pseudotachylytes produced during coseismic slip are ubiquitous within the rocks of the Alpine Fault zone, New Zealand. Pseudotachylytes from three principal host rocks are described and characterised from field and ...

Campbell Island, New Zealand’s southernmost island, is located approximately 700 km south of the South Island at 52.33˚S, 169.09˚E. In February 2009, the R/V Polaris II (Otago University’s research vessel) travelled to ...