Trace-element partition coefficients in the calcite-water system and their paleoclimatic significance in cave studies-Reference-Cited by-同舟云学术

Trace-element partition coefficients in the calcite-water system and their paleoclimatic significance in cave studies

Published:1983-02 Issue:1-3 Volume:61 Page:213-222
ISSN:0022-1694
Container-title:Journal of Hydrology
language:en
Short-container-title:Journal of Hydrology

Author:

Gascoyne Melvyn

Publisher

Elsevier BV

Subject

Water Science and Technology

Reference18 articles.

1. Coprecipitation of manganese and strontium with calcite;Bodine,1965

2. The distribution of solute in crystals grown from the melt, Part I;Burton;Theor. Int. J. Chem. Phys.,1953

3. Coprecipitation of zinc with calcium carbonate;Crocket;Geochim. Cosmochim. Acta,1966

4. Experimentally determined homogeneous distribution coefficients for precipitated magnesium calcites: application to marine carbonate cements;Fuchtbauer,1976

5. Pleistocene Paleoclimates Determined from Stable Isotope and Geochronologic Studies of Speleothem;Gascoyne,1980

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