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The first-order crustal structure of the Magadan region and northeast Sakha Republic (Yakutia), northeast Russia, is obtained by simultaneously inverting for origin times and travel time curves. A total of 1210 observations are used. As an average, a 37-km-thick, 5.992 ± 0.007 km/s crust overlying an 7.961 ± 0.015 km/s mantle provides an excellent fit to phase data listed in the Materialy po Seismichnosti...
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