Sentence examples for maximum subsidence of from inspiring English sources

The maximum subsidence of 0.99 mm is observed at 4.54 m left to the escape tunnel centreline whereas the maximum subsidence of 3.14 mm is observed at 8.89 m right to the main tunnel centreline.

For 2005 2010, records show a maximum subsidence of 630 mm (126 mm/year) in this area.

Shemshaki et al. [26] reported that during 1995 2003, maximum subsidence of 1710 mm occurred in Tehran.

For the Seto Inland Sea region, this resulted in maximum subsidence of about 1 m, and such crustal subsidence effectively increased the height of the tsunamis.

The computed seafloor deformation from the slip model generates a maximum subsidence of approximately 1.22 m and uplift of 0.10 m (Fig. 3b).

In conclusion, for 1992 2005, maximum subsidence of 2050 mm was measured at the same place with maximum subsidence during 1992 2001 (i.e. Yaft Abad). Figure 8 illustrates subsidence in this period.

While several parameters in the model are not well constrained (e.g., initial temperatures of the pyroclastic flow or ground), the results, given a range of plausible parameters, provide a maximum subsidence rate of a few centimeters per year and show how the rate decays to a fraction of a centimeters per year after about 10 months.

Notably, the cumulative thickness of SP III to SP V is thickest near the northeastern and southwestern strike-slip margins, suggesting migration of the loci of maximum subsidence from the normal fault margins towards the strike-slip margins after deposition of SP II.

The regions of maximum subsidence rate correspond to the areas of the thickest pyroclastic deposits and the most extensive fracture networks, i.e., regions A (e.g., Fig.  3a, e) and B (Figs.  3b d and 4).

This paper presents an universal tool for the estimation of maximum subsidence (SMax).

Figures 15 and 16 contain the curves of maximum subsidence and maximum horizontal displacement plotted against bedrock thickness.