|
Resolution: standard / high Figure 3.
Comparison of δ34S in ice-core and snow samples collected from Upper Fremont Glacier with δ34S values of potential sulfate sources to the Wind River Range, Wyoming. Data for comparisons compiled from [5,40-45].
Naftz et al. Geochemical Transactions 2011 12:4 doi:10.1186/1467-4866-12-4 |
