About a relationship between the change of ecological setting of the Black Sea region and the cycles of solar luminosity after the Last Glacial maximum

by Slavova, K.
Source: 1. Mineralia slovaca 1. 0369-2086 1. Roč. 38, č. 4 (2006)
2. [Príl.] Geovestník 2. 0369-2086 2. Č. 4 (2006), s. 11-12

The transition of the Black Sea system from a fresh-water lake to a marine environment at the boundary Lower/Middle Holocene

by Slavova, K.
Source: 1. Mineralia slovaca 1. 0369-2086 1. Roč. 39, č. 2 (2007)
2. [Príl.] Geovestník 2. 0369-2086 2. Č. 2 (2007), s. 16

The fluctuations of the Black Sea Basin after the Last Glacial maximum to 7500 cal. yrs BP as a result of solar luminosity cycles

by Slavova, K., Dimitrov, D.
Source: 1. Mineralia slovaca 1. Roč. 41, č. 3 (2009) 1. 0369-2086
2. Príl.: 2. Geovestník 2. Č. 3 (2009), s. 369

Ancient coastlines of the Black Sea and conditions for human presence

by Dimitrov, D., Slavova, K., Dimitrov, P.
Source: 1. Mineralia slovaca 1. Roč. 41, č. 3 (2009) 1. 0369-2086
2. Príl.: 2. Geovestník 2. Č. 3 (2009), s. 354-355