DEEP SEISMIC SOUNDING ALONG THE OLGUIDAKH-MIRNYI-LENSK PROFILE

dc.contributor.authorSuvorov V.D.
dc.contributor.authorSeleznev V.S.
dc.contributor.authorSolov'ev V.M.
dc.contributor.authorUarov V.F.
dc.contributor.authorKreinin A.B.
dc.date.accessioned2020-02-13T07:44:00Z
dc.date.available2020-02-13T07:44:00Z
dc.date.issued1983
dc.description.abstractThe 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.
dc.identifierhttps://elibrary.ru/item.asp?id=21989147
dc.identifier.citationГЕОЛОГИЯ И ГЕОФИЗИКА, 1983, 24, 9, 72-80
dc.identifier.issn0016-7886
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/15756
dc.titleDEEP SEISMIC SOUNDING ALONG THE OLGUIDAKH-MIRNYI-LENSK PROFILE
dc.typeСтатья

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