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• W2015652987 abstract "At 04:35 on Saturday 4 September 2010 local time (16:35 on 3 September UT) a moment magnitude ( Mw ) 7.1 earthquake struck approximately 10 km southeast of the town of Darfield and within 40 km of New Zealand's second largest city, Christchurch, causing extensive damage in the city and surrounding region. There was no loss of life due to a fortunate combination of strict building codes and the earthquake occurring at 04:35 local time when the streets were largely empty, but about 100 people were injured (two seriously) and many more were made homeless, at least temporarily. Current estimates put the total cost of repairs at NZ $4 billion (about US $3 billion).The key seismological features of the Darfield earthquake are summarized in Table 1. The epicenter and depth are very well constrained by the large number of nearby seismograph and strong-motion accelerometer sites (Figure 1). A surface rupture consistent with strike-slip faulting was quickly identified about 4 km south of the epicenter on a previously unknown fault, which has been named the Greendale fault, although various geophysical data sets have shown that the overall rupture process is more complex.View this table: TABLE 1 The Key Seismological Features of the Darfield Earthquake Modern buildings in Christchurch performed very well in the earthquake, but many older brick and masonry buildings were badly damaged. Liquefaction and the associated lateral spreading and slumping caused extensive damage, even to new buildings, in areas near the coast with sandy soils (Cubrinovski and Green 2010). The earthquake was felt throughout the entire South Island and a large part of the North Island at distances greater than 900 km, with the maximum felt intensity estimated to be Modified Mercalli (MM) 9. Measured accelerations near source exceeded 1 g with several reading well over 0.5 g. A feature of the …" @default.
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• W2015652987 date "2011-05-01" @default.
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• W2015652987 title "The Darfield (Canterbury, New Zealand) Mw 7.1 Earthquake of September 2010: A Preliminary Seismological Report" @default.
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• W2015652987 doi "https://doi.org/10.1785/gssrl.82.3.378" @default.
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