Constraining groundwater flow in the glacial drift and saginaw aquifers in the Michigan Basin through helium concentrations and isotopic ratios
Author:
Affiliation:
1. Department of Earth and Environmental Sciences University of Michigan Ann Arbor MI USA
2. GEOTOP and Département des Sciences de la Terre et de l'Atmosphère Université du Québec à Montréal Montréal QC Canada
Funder
National Science Foundation
Publisher
Wiley
Subject
General Earth and Planetary Sciences
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1111/gfl.12133
Reference96 articles.
1. Determining paleotemperature and other variables by using an error-weighted, nonlinear inversion of noble gas concentrations in water
2. BartonGJ MandleRJ BaltusisMA(1996)Predevelopment freshwater heads in the glaciofluvial Saginaw and Marshall aquifers in the Michigan Basin Open‐ File Report. U.S. Geological Survey Branch of Information Services [distributor] pp. iv 15 pp. Illinois maps 28 cm.
3. Isotopic fractionation of helium during solution: A probe for the liquid state
4. Natural distribution of cosmic-ray produced tritium. II
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