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Botanicheskie Materialy Otdela Sporovyh Rastenij Botanicheskogo Instituti Imeni V.L.

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The standard deviation divided by the average slip value) is also computed for each subfault parameter (further details in Methods section). Earthquake 3d enhanced edition v355. In this analysis the coefficient of variation (i.e. We assess the dispersion of the model parameters around their average values by performing an a-posteriori analysis of the explored models ensemble so that the error associated to each parameter is its weighted standard deviation,. The 2011 Tohoku earthquake slip distribution The slip distribution of the 2011 Tohoku earthquake () extends mainly along strike from ~36.5°N to ~39.5°N and up-dip from the hypocentre in the SE direction (from ~142°E to ~144°E).

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