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As can be seen from the geomorphology map (Fig. 5), the 527 Fault is characterized by significant subsidence in the western fault zone and less subsidence toward the eastern fault zone.
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The subsidence increased toward the northeast part of the area, which is attributed to the mainshock of the 2011 earthquake.
Perhaps the most important finding is the time-dependent stem subsidence rate diminishes toward the end of the experiment, suggesting a stable situation.
The subsidence profiles also shift toward the lower side and more and more significant subsidence occurs beyond the lower panel edge.
The tectonic pulses and flower faults striking to the NW, with antithetic branches continuously reactivating in the study time interval, caused subsidence and basin margin steepening toward the northeast.
A typical fast initial stem subsidence rate, which gradually diminished toward the end of the experiment, was observed (Fig. 4).
The primary natural source of surface O3 is the subsidence of stratospheric O3 from the upper atmosphere toward Earth's surface.
The basement floor is relatively flat but deepens toward the northwestern rim, demonstrating asymmetric subsidence structure.
In both cases of fitting, an almost vertical dike directed toward MEA was estimated to reproduce subsidence in the summit direction at MEA.
We suggest that subsidence of the stem gradually presses the cement toward the periphery of the medullary canal, which leads to cement creep.
SP IV consists of braided-stream conglomerates, suggesting gradual progradation of coarse-grained fluvial systems toward the basin when the extension and subsidence of the basin was slowed.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com