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The reflective zones we found are likely located close to the down-dip end of this locked zone (Fig. 4b).
The locations of the interferogram fringe offsets are consistent with the positions of the strike-slip and normal faulting zones we found in the field (Fig. 2a).
The reflective zones we found are likely located at the down-dip end of the locked zone, where high slip deficit rates are currently observed.
On the arc side of the basin of the subduction and initial collision zones, we found relatively undisturbed strata, showing little arc deformation.
The reflective zones we found are likely located at the down-dip end of the locked zone where high slip deficit rates are currently observed, which may suggest that the reflective zone with high water content delimits the down-dip end of the coseismic rupture zone.
While the highest rates of denitrification were observed in wetter portions of the landscape, including riparian zones, we found that the shallow saturated zone beneath drier upland soils contributed to a larger portion of whole-catchment denitrification due to a larger areal extent.
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However, between group comparisons of the odds ratio for the poor and poorest in the Northern and Coastal zones, we find no significant differences, although the odds were higher in the Northern zone.
Note that the reflective zone we found is located at the down-dip end of the strongly coupled plate boundary.
In that seismic zone, we found two areas where the aftershock was inactive, corresponding to the Aso and the Kuju volcanoes.
Back at the J-Village, on the edge of the exclusion zone, we found out what may motivate some of these men to risk their lives in what must surely be one of the most hostile working environments on earth.
On the other hand, in the rocky zone, which provides a more complex bottom environment than a pebbly zone, we found that individuals had a deep and laterally compressed body with a long head.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com