How large peak ground acceleration by large earthquakes could generate turbidity currents along the slope of northern Japan Trench
Abstract Deep-sea turbidite has been used to determine the history of occurrence of large earthquakes. Surface-sediment remobilization is a mechanism of the generation of earthquake-induced turbidity currents. However, the detailed mechanism of surface-sediment remobilization caused by earthquake gr...
| Published in: | Progress in Earth and Planetary Science |
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| Main Authors: | , , |
| Format: | Article |
| Language: | English |
| Published: |
SpringerOpen
2023-02-01
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| Subjects: | |
| Online Access: | https://doi.org/10.1186/s40645-023-00540-8 |