Abstract:
In Moldova are well known two strips reef is in the north-east and north-west of Moldova, known as Strip Chişinău-Kamenka reef and Moldovan Toltrels. In the present paper is a presentation and an analysis of the genesis of reef formations from northeast of Moldova, the factors that contributed to the formation of coral limestone, geological structure of the region and characterization of Neogene sediments layers of this sector. Has been described and presented graphically their geological sections and the location on the map of outcrops of the strip, some of which are operated by the mining industry from our country.