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This paper presents a detailed geotechnical characterization of pond ashes collected from Panki and Panipat thermal power plants which comes under seismic zone III and IV respectively.
In the present study, geotechnical characterization of pond ash samples collected from Panki and Panipat thermal power plants under seismic zone III and IV respectively have been reported.
In the present study pond ash samples has been collected from two different seismic zone sites in India namely Panki thermal power station (Kanpur, Uttar Pradesh) and Panipat thermal power station (Panipat, Haryana) sites which comes under seismic zone III and IV respectively (IS:1893-Part 1 [11]).
The region falls under Seismic Zone III, which is moderately vulnerable to earthquakes.
According to the Bureau of Indian Standards, the town falls under seismic zone 3, in a scale of 2 to 5 (in order of increasing vulnerability to earthquakes).
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According to the Bureau of Indian Standards, the town falls under seismic zone-IV, (on a scale of I to V, in order of increasing proneness to earthquakes) near the convergent boundary of the Indian and the Eurasian tectonic plates and is subject to frequent earthquakes.
According to the Bureau of Indian Standards, the town falls under seismic zone-IV (on a scale of I to V, in order of increasing seismic activity), near the convergent boundary of the Indian and the Eurasian tectonic plates and is subject to frequent earthquakes.
More recent magnetic surveys show that the structure is a 500-million year-old strike-slip fault, which starts under the Eastern Tennessee Seismic Zone and runs to the eastern coast.
Thus, the purpose of this study is twofold: (i) to validate the suitable static method for zipper column design through nonlinear time-history analyses and; (ii) to investigate the inelastic behavior of the 4-, 8- and 12-storey E-ZBF buildings located in a high risk seismic zone (Victoria, BC) under crustal, subduction, and near-field ground motion ensembles.
Goa forms part of moderate seismic zone in the country, namely, zone III of seismic zoning map of India.
Under the eastern Aleutians, the Wadati Benioff zone also comprises the double seismic zone, with a slightly smaller separation between the upper and lower planes than that of the NE Japan slab. Figure 5b again shows that the estimated dehydration reaction boundaries roughly correspond to the upper and lower seismic planes.
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