Effect of temperature on the transformation of amorphous calcium magnesium carbonate with near-dolomite stoichiometry into high Mg-calcite

Author:

Purgstaller Bettina1234ORCID,Mavromatis Vasileios56789,Goetschl Katja E.1234,Steindl Florian R.1234,Dietzel Martin1234

Affiliation:

1. Institute of Applied Geosciences

2. Graz University of Technology

3. 8010 Graz

4. Austria

5. Geosciences Environment Toulouse (GET)

6. Observatoire Midi-Pyrénées

7. Université de Toulouse

8. CNRS

9. IRD

Abstract

Amorphous calcium magnesium carbonate (ACMC) transformation into high Mg-calcite (HMC) proceeds via dissolution and re-precipitation at the ACMC-solution interface.

Funder

Austrian Science Fund

Deutsche Forschungsgemeinschaft

Publisher

Royal Society of Chemistry (RSC)

Subject

Condensed Matter Physics,General Materials Science,General Chemistry

Reference58 articles.

1. J. W. Morse and F. T.Mackenzie , in Developments in Sedimentology 48 , Elsevier , 1990 , p. 725

2. R. J. Reeder , in Reviews in Mineralogy , Mineralogical Society of America , 11th edn, 1990 , p. 399

3. F. T. Mackenzie , W. D.Bischoff , F. C.Bishop , M.Loijens , J.Schoonmaker and R.Wollast , Carbonates Mineral. Chem. , 1983 , pp. 97–144

4. Mineralogy, nucleation and growth of dolomite in the laboratory and sedimentary environment: A review

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