Group 1 - New Zealand and US researchers are utilizing borehole sensor technology to monitor "slow slip earthquakes" in the Hikurangi subduction zone, enhancing earthquake disaster prevention capabilities [1] - The next step involves publishing seismic sensor data from the Hikurangi subduction zone, which will facilitate a deeper analysis of the overall fault zone risk [1] - The research aims to expand understanding of key faults in the Pacific Ring of Fire, providing new insights for earthquake disaster prevention [1]

Core Insights - New Zealand and US researchers are utilizing borehole sensor technology to monitor "slow slip earthquakes" in the Hikurangi subduction zone, enhancing earthquake disaster prevention capabilities [1] Group 1: Research Findings - "Slow slip earthquakes" are a recently discovered geological phenomenon that differ from traditional earthquakes, with energy release occurring over days or weeks, described as "ripples on the plate interface" [1] - Research indicates that "slow slip earthquakes" can periodically relieve tectonic pressure, playing a crucial role in pressure release during earthquake cycles [1] Group 2: Future Directions - Researchers plan to publish seismic sensor data from the Hikurangi subduction zone and conduct in-depth analysis of the overall fault zone risk [1] - The study aims to expand understanding of key faults in the Pacific Ring of Fire, providing new insights for earthquake disaster prevention [1]