PETROGENESIS OF AUTOLITHS FROM KIMBERLITIC BRECCIAS IN THE V. GRIB PIPE (ARKHANGELSK DISTRICT)

dc.contributor.author	Golubeva Yu.Yu.
dc.contributor.author	Pervov V.A.
dc.contributor.author	Kononova V.A.
dc.date.accessioned	2024-11-02T11:07:43Z
dc.date.available	2024-11-02T11:07:43Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13520941
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 8, 1257-1262
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46331
dc.description.abstract	Kimberlitic diatremes are primarily composed of autolithic kimberlitic breccia. The name of this variety of kimberlitic rocks is related to the specific distribution of autoliths in the matrix. Autoliths are prominent fragments of kimberlitic breccia. The autoliths are also known as kimberlite-type inclusions in kimberlite, inclusions of kimberlites of earlier generations, fragments of magmatic kimberlite, pellets, and lapillies. The shape of these rocks can be both rounded (the shell smoothes out the irregular surface of the core) and irregular (with inlets and projections).
dc.subject	kimberlitic breccia
dc.subject	Grib pipe
dc.title	PETROGENESIS OF AUTOLITHS FROM KIMBERLITIC BRECCIAS IN THE V. GRIB PIPE (ARKHANGELSK DISTRICT)
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06080228

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