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using local arrays of recorders, while the deeper layers have been investigated using global networks to detect seismic signals that have traversed the interior of the Earth The continental crust was discovered by Andrija Mohorovicic from studies of the seismic waves gener ated by the Croatia earthquake of 1909 (Fig 214) Within a range of about 200 km from the epicenter, the rst seismic arrivals were P waves that traveled directly from the focus to the recorders with a velocity of 56 km s 1 This seismic phase was termed Pg At greater ranges, however, P waves with the much higher velocity of 79 km s 1 became the rst arrivals, termed the Pn phase These data were interpreted by the standard techniques of refraction seismology, with Pn representing seismic waves that had been critically refracted at a velocity discontinuity at a depth of some 54 km. asp.net gs1 128 EAN - 128 ASP . NET Control - EAN - 128 barcode generator with free ...
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ASP . NET GS1 128 Generator WebForm Control to generate GS1 EAN-128 in ASP.NET projects. Download Free Trial Package | Include developer guide ... This discontinuity was subsequently named the Mohorovicic discontinuity, or Moho, and it marks the boundary between the crust and mantle Subsequent work has demonstrated that the Moho is universally present beneath continents and marks an abrupt increase in seismic velocity to about 8 km s 1 Its geometry and re ective character are highly diverse and may include one or more sub-horizontal or dipping re ectors (Cook, 2002) Continental crust is, on average, some 40 km thick, but thins to less than 20 km beneath some tectonically active rifts (eg Sections 73, 781) and thickens to up to 80 km beneath young orogenic belts (eg Sections 1024, 1045) (Christensen & Mooney, 1995; Mooney et al, 1998) A discontinuity within the continental crust was discovered by Conrad in 1925, using similar methods. asp.net gs1 128 Packages matching Tags:"Code128" - NuGet Gallery
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