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How These Oddly Contorted Oceanic Plate Triggered a Complex Earthquake in New Zealand

A research team led by the University of Tsukuba used seismic data generated by a magnitude 7.3 earthquake that struck off the northeasternmost tip of New Zealand's North Island on March 4, 2021.

Contorted oceanic plate caused complex quake off New Zealand s East Cape

New model reveals previously unrecognized complexity of oceanic earthquake zones

 E-Mail IMAGE: Overview of the study area and the schematic illustration of interaction of fault motion and the seafloor subsidence. view more  Credit: University of Tsukuba Tsukuba, Japan - Researchers from the University of Tsukuba applied seismic data from around the world to build a model of the 2020 Caribbean earthquake. Oceanic transform faults are generally considered to be linear and simple and have been widely used in studies of earthquake dynamics. However, the research team found that high complexity in rupture speed and direction can occur even in a supposedly simple linear fault system. On 28 January 2020, a large oceanic earthquake with magnitude 7.7 occurred at the Oriente transform fault in the Caribbean Sea, between Jamaica and Cuba. It caused a minor tsunami of 0.11 m height and was felt as far afield as Florida.

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