О ВОЗМОЖНОСТИ РАЗВИТИЯ ДОКАЙНОЗОЙСКОГО КАРБОНАТНОГО ТРОПИЧЕСКОГО КАРСТА В НЕЧЕРНОЗЕМЬЕ

dc.contributor.author	Лукашов А.А.
dc.contributor.author	Иксанова Е.А.
dc.date.accessioned	2022-12-03T09:10:06Z
dc.date.available	2022-12-03T09:10:06Z
dc.date.issued	2005
dc.identifier	https://www.elibrary.ru/item.asp?id=9142771
dc.identifier.citation	Геоморфология, 2005, , 2, 52-57
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/40701
dc.description.abstract	Karst topography was developed in the center of the Russian Plain during the end of Paleozoic and the beginning of Mesozoic. Reconstruction of paleorelief within the bound of Moscow shows that tropical karst topography was spread on the territory of interfluves.
dc.title	О ВОЗМОЖНОСТИ РАЗВИТИЯ ДОКАЙНОЗОЙСКОГО КАРБОНАТНОГО ТРОПИЧЕСКОГО КАРСТА В НЕЧЕРНОЗЕМЬЕ
dc.type	Статья
dc.subject.udc	551.4.07:551.435.8(470.1/.6)

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