Open access
Aug 2026
Oxygen Isotopic Composition of Miocene Meteoric Water (δ18Ow) in Alpine Foreland Basins
The reconstructed stable oxygen isotopic composition of meteoric water (δ18Ow) is widely used for paleoclimate reconstructions. Understanding past environmental factors that drove changes in δ18Ow is essential for interpreting past climate conditions. Here, we investigate the spatial and temporal variations of δ18Ow in...
Armelle Ballian, M. Meijers, D. Boateng et al.
· Geochemistry Geophysics Geos... · 0 citations