Sandstones and conglomerates formed by precipitation of CaCO3 under stagnant ice sheet
Quaternary sandstones and conglomerates found on the valley-sides of the lower Vistula River have been identified as a product of precipitation of CaCO3 under stagnant Middle-Vistulian ice sheet. The trigger mechanizm of precipitation of CaCO3 has
Quaternary sandstones and conglomerates found on the valley-sides of the lower Vistula River have been identified as a product of precipitation of CaCO3 under the stagnant Middle-Vistulian ice sheet. The model of precipitation of CaCO3 is attributed