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The hypocentral depth was very shallow, less than five kilometers.
The earthquake had a maximum slip of 14 m in the hypocentral region.
The hypocentral depth is estimated as 8 km from body wave modelling.
This occurs directly beneath the epicenter, at a distance known as the focal or hypocentral depth.
The hypocentral region of this earthquake extended from offshore Iwate Prefecture to offshore Ibaraki Prefecture.
The hypocentral region of Sanriku coastal earthquakes can occur in locations extending from offshore Aomori Prefecture to offshore Ibaraki Prefecture.
By selecting the epicenter, the earthquake information includes the event date, time, location coordinates in degrees latitude and longitude, and hypocentral depth in kilometers; selecting a seismic station jumps to that stations entry in the table.
Examples include the hypercentral groups whose transfinite upper central series form such a central series, as well as the hypocentral groups whose transfinite lower central series form such a central series .
The reason for so many different ways to measure the same thing is that at different distances, for different hypocentral depths, and for different earthquake sizes, the amplitudes of different types of elastic waves must be measured.
Earthquake focal mechanisms and hypocentral depths show that shortening is accommodated by a mixture of high-angle and low-angle reverse faulting, within either the lowest part of the sedimentary cover or in the basement beneath the Hormuz salt.
The DD technique takes advantage of the fact that if the hypocentral separation between two earthquakes is small compared to the event-station distance and the scale length of velocity heterogeneity, then the ray paths between the source region and a common station are similar along almost the entire ray path (Frechet, 1985; Got et al., 1994).