Mineralogeneza formaţiunilor geologice din cadrul segmentului moldovenesc a bazinului râului Nistru [Articol]

Abstract

This paper presents a geological synthesis of data from geological reports in the collection of the Agency for Geology and Mineral Resources. The segment of the Dniester River basin within the northeastern territory of the Republic of Moldova has always been an object of mineralogical study, carried out both for the purpose of establishing the geological evolution of the Precambrian and for the purpose of determining the geological-economic perspective of the Precambrian sedimentary and crystalline formations in this region. Geological mapping and prospecting were carried out in the last decades of the last century, based on three main geological factors – the shallow depth to the surface of the platform base consisting of Archeanroterozoic crystalline rocks, the presence of a disjunctive tectonic structure – the Dniester Fault and the presence of isolated metalliferous mineralization in the Ediacaran basal strata.