CONODONTS IN XENOLITHS OF SEDIMENTARY ROCKS FROM KIMBERLITE PIPES OF THE DALDYN-ALAKIT AREA (SAKHA)

dc.contributor.authorTarabukin V.P.
dc.date.accessioned2021-11-21T03:19:35Z
dc.date.available2021-11-21T03:19:35Z
dc.date.issued2003
dc.description.abstractDiverse conodont assemblages discovered in xenoliths of sedimentary rocks from kimberlite pipes are analyzed and correlated with zonal stratigraphic scales. Based on the original and published data, a Paleozoic rock sequence that existed in the area at the stage of pipe formation is reconstructed, and its stratigraphic hiatuses serving as criteria for exploration of diamonds are distinguished.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13419446
dc.identifier.citationStratigraphy and Geological Correlation, 2003, 11, 2, 199-208
dc.identifier.issn0869-5938
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/32267
dc.subject.agePaleozoic
dc.subject.ageПалеозойru
dc.titleCONODONTS IN XENOLITHS OF SEDIMENTARY ROCKS FROM KIMBERLITE PIPES OF THE DALDYN-ALAKIT AREA (SAKHA)
dc.typeСтатья

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