Abstract
A total of 129 samples of tsunami deposits were collected immediately after the 2011 off the Pacific coast of Tohoku Earthquake at 5 km intervals over the 250 km length of the tsunami inundation zone. They were analyzed for 10 major rock-forming elements, arsenic, and base metals (Cu, Zn, Pb, and Cd) with EDXRF. Statistical analysis indicates that the populations of arsenic and heavy metals—with the exception of Cd, which had values below the detection limit—comprise two log-normal distributions divided by a threshold value: 89 ppm Cu, 245 ppm Zn, 48 ppm Pb, and 21 ppm As. Spider diagrams of their anomalous values normalized by average marine sediments in Sendai bay indicate a characteristic pattern in each mineralization province. They are coincident to river sediment anomalies detected before the tsunami and are also compatible with the production of disused mines located in the background area. We conclude that almost all base metals and arsenic anomalies in the tsunami deposits distributed on the Sanriku coast and Sendai Plain by the 2011 off the Pacific coast of Tohoku Earthquake are affected by specific geological and mineralogical properties.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
