DEEP SEISMIC SOUNDING ALONG THE OLGUIDAKH-MIRNYI-LENSK PROFILE

Abstract

The structure of the crust and the Moho surface along a profile intersecting the Mirny kimberlite field is considered. Revealed heterogeneous structure of the crust and upper mantle. It is assumed that the selected seismic anomalies reflect the deep manifestation of kimberlite magmatism.