Cross-Formational Flow and Salinity Sources Inferred From a Combined Study of Helium Concentrations, Isotopic Ratios, and Major Elements in the Marshall Aquifer, Southern Michigan
Geochemistry, Geophysics, Geosystems - United States
doi 10.1029/2005gc001010
Full Text
Open PDFAbstract
Available in full text
Date
October 1, 2005
Authors
Publisher
American Geophysical Union (AGU)