Strontium isotopes as indicators of the dissolving phase in a carbonate aquifer: implications for 14C dating of groundwater-Reference-Cited by-同舟云学术

Strontium isotopes as indicators of the dissolving phase in a carbonate aquifer: implications for 14C dating of groundwater

Published:1994-02 Issue:1-4 Volume:154 Page:301-321
ISSN:0022-1694
Container-title:Journal of Hydrology
language:en
Short-container-title:Journal of Hydrology

Author:

Bishop P.K.,Smalley P.C.,Emery D.,Dickson J.A.D.

Publisher

Elsevier BV

Subject

Water Science and Technology

Reference42 articles.

1. 234U238U activity ratios of dissolved uranium in groundwaters from a Jurassic Limestone aquifer in England;Andrews;Earth Planet. Sci. Lett.,1982

2. Dissolved gases as indicators of groundwater mixing in a Jurassic Limestone aquifer;Andrews,1980

3. Carbonate sediments and their diagenesis;Bathurst;Devel. Sedimentol.,1975

4. Carbon isotope hydrogeochemistry of the Lincolnshire Limestone formation, England, with special reference to sample preparation and analysis;Bishop,1988

5. Precipitation of dissolved carbonate species from natural waters for δ13C analysis — A critical appraisal;Bishop;Chem. Geol. (Isot. Geosci. Sect.),1990

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