Thallium stable isotope ratio and mass fraction measurements were performed on sixteen geological reference materials spanning three orders of magnitude in thallium mass fraction, including both whole-rock and partially-separated mineral powders. For stable isotope ratio measurements, a minimum of three independent digestions of each reference material were obtained. High-precision trace element measurements (including Tl) were also performed for the majority of these RMs. The range of Tl mass fractions represented is 10 ng g -1 to 16 μ g g -1 , and Tl stable isotope ratios (reported for historical reasons as ε 205 Tl relative to NIST SRM 997) span the range -4 to +2. With the exception – attributed to between-bottle heterogeneity – of G-2,...
Stable thallium (Tl) isotopes are an extremely sensitive tracer for the addition of small amounts of...
Thallium is a complex and intriguing heavy element, having both chalcophile and lithophile character...
Author Posting. © The Author(s), 2012. This is the author's version of the work. It is posted here ...
Thallium stable isotope ratio and mass fraction measurements were performed on sixteen geological re...
Thallium stable isotope ratio and mass fraction measurements were performed on sixteen geological re...
This contribution summarizes the current state of understanding and recent advances made in the fiel...
Stable thallium (Tl) isotopes are an extremely sensitive tracer for the addition of small amounts of...
We present optimised analytical protocols for the precise and accurate determination of Tl concentra...
The Bingham Canyon porphyry deposit is one of the world’s largest Cu-Mo-Au resources. Elevated conce...
The Bingham Canyon porphyry deposit is one of the world’s largest Cu-Mo-Au resources. Elevated...
Thallium is a highly poisonous heavy metal. Since Tl pollution control has been neglected worldwide ...
Lead-205 decays to 205Tl with a half-life of 15 Myr and should have been present in the early solar ...
Continental weathering plays a key role in modifying the geochemical budget of terrestrial reservoir...
The isotope composition of Ph is difficult to determine accurately due to the lack of a stable norma...
We present a concerted international effort to cross-calibrate five synthetic Th isotope reference m...
Stable thallium (Tl) isotopes are an extremely sensitive tracer for the addition of small amounts of...
Thallium is a complex and intriguing heavy element, having both chalcophile and lithophile character...
Author Posting. © The Author(s), 2012. This is the author's version of the work. It is posted here ...
Thallium stable isotope ratio and mass fraction measurements were performed on sixteen geological re...
Thallium stable isotope ratio and mass fraction measurements were performed on sixteen geological re...
This contribution summarizes the current state of understanding and recent advances made in the fiel...
Stable thallium (Tl) isotopes are an extremely sensitive tracer for the addition of small amounts of...
We present optimised analytical protocols for the precise and accurate determination of Tl concentra...
The Bingham Canyon porphyry deposit is one of the world’s largest Cu-Mo-Au resources. Elevated conce...
The Bingham Canyon porphyry deposit is one of the world’s largest Cu-Mo-Au resources. Elevated...
Thallium is a highly poisonous heavy metal. Since Tl pollution control has been neglected worldwide ...
Lead-205 decays to 205Tl with a half-life of 15 Myr and should have been present in the early solar ...
Continental weathering plays a key role in modifying the geochemical budget of terrestrial reservoir...
The isotope composition of Ph is difficult to determine accurately due to the lack of a stable norma...
We present a concerted international effort to cross-calibrate five synthetic Th isotope reference m...
Stable thallium (Tl) isotopes are an extremely sensitive tracer for the addition of small amounts of...
Thallium is a complex and intriguing heavy element, having both chalcophile and lithophile character...
Author Posting. © The Author(s), 2012. This is the author's version of the work. It is posted here ...