i) d col pg) thiu elu nal tio pr S (A e w da od m y o ns o Lithium isotopes have the potential to provide insights into tion of d Li and Li/Ca record of long-term evolution of seawater hydrothermal weathering.12–16 High precision lithium isotope ratio measurements have been onization mass spectrometry,17–20 by quadrupole ICP-MS by MC-ICP-MS (0.2 & to surements are susceptible to igh concentrations of matrix ver, ICP-MS methods are also zation interferences caused by elements. TIMS methods are tant instrumental fractionation mass requirement (>100 ng), 0 pg level) and variable matrix TIMS requires quantitative lements and filament loading of (Li-borate or Li-phosphate). ment during TIMS analyses ha
Lithium (Li) and strontium (Sr) are two economically relevant chemical elements whose oceanic biogeo...
A comprehensive understanding of lithium-isotope fractionation during terrestrial weathering is nece...
The distribution of Li isotopes in pore waters to a depth of 1157 m below seafloor is presented for ...
We present an improved method for lithium isotope ratio (7Li/6Li) determinations with low total lith...
International audienceWe report here a newly developed method for measurement of Li isotopes by use ...
International audienceIn this study, the accuracy and the precision corresponding to Li isotopic mea...
Accurate determination of lithium (Li)isotopic composition in natural geological samples is the basi...
This manuscript is a summary of the research work carried out at BRGM over the past 10 years under m...
The low temperature realm such as the geothermal systems, characterized by a large variety of near-E...
An improved procedure for lithium isotope analysis using Li3PO4 as the ion source has been investiga...
The accurate determination of Li isotopic ratios by MC-ICP-MS has traditionally been hampered by the...
International audienceIn this study, to better understand the factors controlling the concentration ...
International audienceThe Li isotope signatures of hydrothermal fluids are remarkably constant (View...
Lithium isotope ratios play a key role in tracing weathering processes within the context of paleocl...
Silicate weathering is a primary control on the carbon cycle and therefore long-term climate. Tracin...
Lithium (Li) and strontium (Sr) are two economically relevant chemical elements whose oceanic biogeo...
A comprehensive understanding of lithium-isotope fractionation during terrestrial weathering is nece...
The distribution of Li isotopes in pore waters to a depth of 1157 m below seafloor is presented for ...
We present an improved method for lithium isotope ratio (7Li/6Li) determinations with low total lith...
International audienceWe report here a newly developed method for measurement of Li isotopes by use ...
International audienceIn this study, the accuracy and the precision corresponding to Li isotopic mea...
Accurate determination of lithium (Li)isotopic composition in natural geological samples is the basi...
This manuscript is a summary of the research work carried out at BRGM over the past 10 years under m...
The low temperature realm such as the geothermal systems, characterized by a large variety of near-E...
An improved procedure for lithium isotope analysis using Li3PO4 as the ion source has been investiga...
The accurate determination of Li isotopic ratios by MC-ICP-MS has traditionally been hampered by the...
International audienceIn this study, to better understand the factors controlling the concentration ...
International audienceThe Li isotope signatures of hydrothermal fluids are remarkably constant (View...
Lithium isotope ratios play a key role in tracing weathering processes within the context of paleocl...
Silicate weathering is a primary control on the carbon cycle and therefore long-term climate. Tracin...
Lithium (Li) and strontium (Sr) are two economically relevant chemical elements whose oceanic biogeo...
A comprehensive understanding of lithium-isotope fractionation during terrestrial weathering is nece...
The distribution of Li isotopes in pore waters to a depth of 1157 m below seafloor is presented for ...