Petrological Summary: Reaction Series Leading from Carbonate Sediments to Carbonate Rocks

  • Friedrich Lippmann
Part of the Minerals, Rocks and Inorganic Materials book series (MINERALS, volume 6)

Abstract

The simplest process of carbonate sedimentation is the precipitation from fresh-water, i.e. from solutions which are so low in dissolved magnesium that calcium is essentially the only important cation susceptible to forming a sparingly soluble carbonate. One of the most important factors determining carbonate solubility in any natural water is the partial pressure of CO2, which acts upon the activity product of the carbonate to precipitate via the equilibria (9), (10), and (11) (p. 103) among the various dissolved species related to the carbonate ion.

Keywords

Magnesium Silicate Lithification Calcite Recrystallization 

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Copyright information

© Springer-Verlag Berlin · Heidelberg 1973

Authors and Affiliations

  • Friedrich Lippmann
    • 1
  1. 1.Mineralogisch-Petrographisches Institut der UniversitätTübingenGermany

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