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GeoRef Categories
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Fukushima Dai-ichi power station
Atmospheric Dispersion and Deposition of Radionuclides from the Fukushima Daiichi Nuclear Power Plant Accident
Fukushima—Two Years Later
Land-Surface Contamination by Radionuclides from the Fukushima Daiichi Nuclear Power Plant Accident
Seismic Damage Indicating Parameters at Nuclear Power Plants Affected by the 2011 Tohoku-Oki Earthquake and Plant Shutdown Criteria
Interactions between Nuclear Fuel and Water at the Fukushima Daiichi Reactors
Examining the Nuclear Accident at Fukushima Daiichi
Oceanic Dispersion Simulations of 137Cs Released from the Fukushima Daiichi Nuclear Power Plant
Time and Space Distribution of Coseismic Slip of the 2011 Tohoku Earthquake as Inferred from Tsunami Waveform Data
Post 23 August 2011 Mineral, Virginia, Earthquake Investigations at North Anna Nuclear Power Plant
MOLECULAR SIMULATION OF CESIUM ADSORPTION AT THE BASAL SURFACE OF PHYLLOSILICATE MINERALS
AIKITU TANAKADATE AND THE CONTROVERSY OVER VERTICAL ELECTRICAL CURRENTS IN GEOMAGNETIC RESEARCH
Seismic risk assessment for the CEUS nuclear power plant fleet based on the NGA-East ground motion model
Christchurch Women's Hospital: Analysis of Measured Earthquake Data during the 2011–2012 Christchurch Earthquakes
Simplified methods to estimate mean hazard due to updated ground motion model: Application to nuclear power plants in CEUS
Abstract Microplastics have become widely dispersed throughout the marine environment in and around Japan since the 1960s, which corresponds to the onset of mass plastic production and use in this country. Our study documents a possible abrupt microplastic depositional event in continental shelf and deep-sea environments triggered by a tsunami. The sediment layers contaminated by microplastics correspond with sedimentary horizons where 137 Cs signals were measured, indicating deposition after 1960s nuclear tests. The microplastics were observed in the 2011 Tohoku-Oki tsunami deposits. Tsunamis can thus contribute to the wide dispersal of microplastics from coastal to deep-sea areas, and these anthropogenic particles can be used to date very recent turbidite deposits.