The increase in marine Li isotope composition (δ 7 Li,∼ 9‰) since the Cenozoic is possibly
related to continental chemical weathering associated with tectonic uplift (eg, the Tibetan …

To examine the alteration of river-derived sediments through a large estuary and the
implications for elemental cycling and global climate, this study analyses lithium (Li) …

The properties of the heat source determine the exploitation potential and scientific research
value of a high-temperature hydrothermal geothermal system. Existing hydrogeochemical …

Chemical weathering is one of the most important processes on the Earth's surface, and
lithium isotopes have been used as a promising tracer of silicate weathering, as the …

To investigate the impact of riverine discharge and weathering intensity on lithium isotopes
(δ 7 Li) in a mono-lithological terrain, this study examines the dissolved load and leached …

Lithium isotope ratios (δ7Li) of rivers are increasingly serving as a diagnostic of the balance
between chemical and physical weathering contributions to overall landscape denudation …

The study of lithium isotopic (δ 7 Li) signatures in sedimentary deposits has become a
powerful tool to infer past silicate weathering regimes, thus informing our knowledge of the …

The shift in Sr stable isotope ratios (88 Sr/86 Sr, reported as δ 88/86 Sr values) in
weathering systems provides insights into the transformation of the binding form of Sr …

Chemical weathering processes play a key role in regulating the global climate over
geological time scales. Lithium (Li) isotope compositions have proven to be a robust proxy …

Lithium (Li) isotopes are widely used as a tracer of silicate weathering. However, Li isotopic
compositions of non-silicate phases carried by sediments/suspended particulate matters …