A slow-slipping earthquake is gaining momentum

Two international science missions, conducted in 2017 and 2018, have allowed scientists to study the biggest mistake in the New Zealand earthquake in the hope of learning more about slow earthquakes in subduction areas around the world.

Researchers from the National Water and Atmospheric Research Institute (NIWA), GNS Science, the University of Texas, and International Ocean Discovery Campaigns (IODP) have led the Hikurangi subduction zone off the east coast of North Island. Oakland University. This research represents the first time that scientists have studied rock samples from the source region for slow slipping events and take samples directly from them by drilling on the ocean floor.

Slow events are similar to regular earthquakes, but instead of sudden and catastrophic energy emitted, slow earthquakes occur in increments that may last from days to months and can repeat every year or two. Niue Principal Scientist Dr. Philip Barnes explains that these events are important not only as a new type of seismic behavior, but because they occur in areas prone to major earthquakes and tsunamis. He added: “Since the slow earthquakes are still only recently discovered, we do not yet understand their relationship to the devastating earthquakes.”

New Zealand has been identified as one of the best places to study such events because they are located near the sea floor, making rigs to collect geophysical information and rock samples a viable option. A cross-section was drilled across the plate boundary off the coast of Gisborne to analyze the properties of the rocks where slipping events occur. “What we believe is that shallow slow slip events occur in fault areas consisting of a mixture of different rocks of different scales, which are highly variable in their composition,” Barnes says.

The study indicates that contradictory types of rocks in areas of rift may lead to both noticeable slow movements, and possibly others, within the limits of subduction around the world. Barnes notes that the research relates not only to New Zealand, but also to other areas prone to seismic behavior, such as those along the Ring of Fire.

Parts of volcanic rock core and rock carbonate collected during IODP 375 flight from the time interval associated with the Hikurangi Slow Slip Fault Zone. © Phil Barnes, Newa

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