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 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.

United statesCaribbean seaBelize generalRyo okuwakiYuji yagiGeophysical research lettersUniversity of tsukubaProfessor yujiProfessor ryoOriente transform faultInvolving supershear ruptureGeometric complexityஒன்றுபட்டது மாநிலங்களில்கரீபியன் கடல்பெலிஸ் ஜநரல்புவி இயற்பியல் ஆராய்ச்சி எழுத்துக்கள்