POLARIZATION AND BISPECTRA OF MICROSEISMS OBSERVED AT THE BOROVOE GEOPHYSICAL OBSERVATORY

Abstract

Results are presented from an analysis of the polarization and bispectra of microseisms recorded during a 1-day noise monitoring session conducted at the Borovoe Geophysical Observatory, Kazakhstan. Some information was derived concerning the origin of some microseism radiation flows produced by a variety of manmade and natural sources.