Recent studies show that high-technology rare earth elements (REEs) of anthropogenic
origin occur in the environment including in aquatic systems, suggesting REEs are …

Abstract Groundwater 18O/16O, 2H/1H, 13C/12C, 3H, and 14C data can help quantify
molecular movements and chemical reactions governing groundwater recharge, quality …

Systematically varying properties and reactivities have led to focused research of the
environmental forensic capabilities of rare earth elements (REE). Increasing anthropogenic …

The depositional environment of sedimentary rocks from the Neoarchaean Fortescue Group
(2.78–2.63 Ga) in the Hamersley Basin, Pilbara Craton, Western Australia, is controversial …

Abstract During the Aptian (Cretaceous), in what is now the South Atlantic, the largest
chemogenic (abiotic) carbonate factory so far identified in the Phanerozoic geological record …

Large oil accumulation discoveries in the last decade in the pre-salt rock succession off the
Brazilian coast aroused renewed interest in carbonate reservoirs, prompting several studies …

Rare earth element (REE) geochemistry is a useful tool in delineating hydrogeochemical
processes and tracing solute transport, which can be used to reveal groundwater chemical …

The present work examines the possible use of major ion chemistry and multivariate
statistical techniques as a rapid and relatively cost‐effective method of identifying the extent …

Groundwater dynamics in continental rift zone settings remain poorly understood because of
the spatial heterogeneity in flow, storage, and recharge dynamics. The Central Kenya Rift is …

The hydrological relationship between surface waters and groundwaters in many regions of
the world is well known and the effects of their mutual interaction and interaction with the …