ЛИЗАРДИТ И САПОНИТ В КИМБЕРЛИТОВОЙ ТРУБКЕ КАТОКА (ЗАПАДНАЯ АФРИКА)

dc.contributor.authorЗинчук Н.Н.
dc.contributor.authorЖухлистов А.П.
dc.contributor.authorКотельников Д.Д.
dc.contributor.authorБ стегницкий Ю.Б.
dc.date.accessioned2024-03-16T02:51:53Z
dc.date.available2024-03-16T02:51:53Z
dc.date.issued2006
dc.description.abstractAn unusual association of simple (1T, 3R) and two complex (nonstandard) orthogonal polytypes of lizardite was found, for the first time, within porphyry kimberlites occurring in volcanogenic-sedimentary rocks. One of the nonstandard polytypes is characterized by the ordered six-layered structure, with the same orientation of adjacent layers, and another one has a semi-ordered six-layered (three-layered) structure with more complicated, than for simple polytypes, regulation in alternating of the contrary-wise oriented layers.
dc.identifierhttps://elibrary.ru/item.asp?id=9222553
dc.identifier.citationЗаписки Российского минералогического общества, 2006, 135, 1, 91-102
dc.identifier.issn0869-6055
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/42988
dc.subject.udc5491548
dc.titleЛИЗАРДИТ И САПОНИТ В КИМБЕРЛИТОВОЙ ТРУБКЕ КАТОКА (ЗАПАДНАЯ АФРИКА)
dc.typeСтатья

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