О ВОЗМОЖНОСТИ РАЗВИТИЯ ДОКАЙНОЗОЙСКОГО КАРБОНАТНОГО ТРОПИЧЕ-- СКОГО КАРСТА В НЕЧЕРНОЗЕМЬЕ

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.