Origin Of Carbonate Sedimentary Rocks Pdf New -

Ca2++2HCO3−⇌CaCO3↓+CO2↑+H2OCa raised to the 2 plus power plus 2 HCO sub 3 raised to the negative power is in equilibrium with CaCO sub 3 down arrow positive CO sub 2 up arrow positive H sub 2 O

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] is rarely precipitated directly by modern organisms or open marine waters. Instead, most dolostones form when magnesium-rich fluids pass through pre-existing limestone during diagenesis, replacing calcium ions with magnesium: replacing calcium ions with magnesium: