Mechanisms of subglacial groundwater recharge as derived from noble gas, 14C, and stable isotopic data
Abstract
Noble gas, stable isotope and 14C data from samples collected along groundwater flow path within a confined Paleozoic aquifer in northeastern Wisconsin, USA are used to deduce the effect of the Laurentide Ice Sheet (LIS) on the underlying groundwater and its recharge dynamics. During the last glacial maximum the investigated area was near the center of the Green Bay Lobe of the LIS. 14C ages that extend to 26 k.a. and low δ18O derived...
Paper Details
Title
Mechanisms of subglacial groundwater recharge as derived from noble gas, 14C, and stable isotopic data
Published Date
May 1, 2013
Volume
369-370
Pages
78 - 85
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