Skip to main content
Earth, Planets and Space
Fig. 3 | Earth, Planets and Space

Fig. 3

From: Heterogeneous mantle anisotropy and fluid upwelling: implication for generation of the 1891 Nobi earthquake

Fig. 3

Polarization data from the research area are shown in four geographic regions (a–d). The polarization azimuths of the maximum-velocity phase and the time delay between the maximum- and minimum-velocity phases are indicated by the direction and length of each bar, respectively. Bars are overlain on locations of seismic stations. Stars denote epicenters of deep earthquakes

Back to article page