Article ID Journal Published Year Pages File Type
8866102 Journal of Geochemical Exploration 2018 13 Pages PDF
Abstract
The stable isotopic data (δ2H and δ18O) fall in the local meteoric water line (LMWL), suggesting current recharge and limited oxygen isotopic exchange during rock-dissolution processes. This could indicate short residence times and/or abundant contribution of actual meteoric water at shallow depths.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Economic Geology
Authors
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