Drilling into a Future Earthquake
Eos,
About every 300 years, the Alpine Fault on New Zealand’s South Island produces a large—approximately magnitude 8—earthquake.
Petrophysical, Geochemical, and Hydrological Evidence for Extensive Fracture‐Mediated Fluid and Heat Transport in the Alpine Fault's Hanging‐Wall Damage Zone
Overview of attention for article published in Geochemistry, Geophysics, Geosystems, December 2017
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