Tectono‐Thermal Evolution of the Hope‐Kelly Fault System, Southern Alps, New Zealand: Insights From Topographic Analysis and (U‐Th)/He Thermochronology
Abstract:The fast‐slipping Alpine (∼30 mm/yr), Hope (∼10–20 mm/yr) and Kelly (∼6 mm/yr) faults in the South Island of New Zealand form a complex intersection zone that accommodates tectonic strain along the Australian‐Pacific plate boundary. Analysis of digital topography reveals evidence for stream capture, drainage divide migration, landscape responses to incipient fault development, and preserved enclaves of relic topography that collectively reflect complex interplays between active faulting and landscape evolution… Show more
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