Overpressured fluids played large role in Kaikōura quake

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New Zealand
Ulrich Lange via Wikimedia Commons
Ulrich Lange via Wikimedia Commons

A study on the 2016 Kaikoura earthquake shows how "overpressured" fluids underground – basically, lots of water molecules trapped under an impermeable layer of rock – likely facilitated the beginning of the quake. The researchers also found that a chunk of earth near Kaikoura may have deflected the rupture to the north, causing it to spread across over 20 faults under land, rather than eastwards, under the sea. They say that similar chunks of earth (known as "high-velocity bodies") have been found at other major quakes such as the 1906 San Fransisco event and the 2010–2011 Darfield-Christchurch sequence.

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Research Elsevier, Web page Open access
Journal/
conference:
Physics of the Earth and Planetary Interiors
Research:Paper
Organisation/s: GNS Science, University of Otago, Victoria University of Wellington, Tohuku University of Japan, Kyushu University of Japan, Kyoto University of Japan, University of Wisconsin-Madison
Funder: New Zealand Earthquake Commission projects 18/753 and 18/755 and the US National Science Foundation awards EAR-1717119 and EAR-1756075.
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