О ВОЗМОЖНОСТИ РАЗВИТИЯ ДОКАЙНОЗОЙСКОГО КАРБОНАТНОГО ТРОПИЧЕСКОГО КАРСТА В НЕЧЕРНОЗЕМЬЕ

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.