Abstract
Susbsystem “Ozherelye” of peripheral points Zerenda, Vostochniy, Chkalovo of the large-base seismic array of Geophysical Observatory “Borovoye” has been studied. At the example of recording of underground nuclear explosions carried out at Nevada Test Site, local travel time curves and linear trends of the P wave travel time at the traces: “Pahute test site – peripheral points Zerenda, Vostochniy, Chkalovo” have been investigated.
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