Kinetic and thermodynamic factors controlling the distribution of SO32− and Na+ in calcites and selected aragonites-Reference-Cited by-同舟云学术

Kinetic and thermodynamic factors controlling the distribution of SO32− and Na+ in calcites and selected aragonites

Published:1985-03 Issue:3 Volume:49 Page:713-725
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Busenberg Eurybiades,Niel Plummer L.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference38 articles.

1. Physical Chemistry of Surfaces;Adamson,1976

2. Distribution and nature of incorporation of trace elements in modern aragonitic corals;Amiel;Sedimentology,1973

3. Biomineralization of crinoid echinoderms: Characterization of skeletal elements using TEM and STEM microanalysis;Blake;Scanning Electron Microscopy,1981

4. The kinetics of dissolution of dolomite in CO2-H2O systems at 1.5 to 65°C and 0 to 1 atm PCO2;Busenberg;Amer. J. Sci.,1982

5. A comparative study of the dissolution and precipitation kinetics of calcite and aragonite;Busenberg;U.S. Geol. Surv. Bull,1985

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