4.7 Article

First vanadium isotope analyses of V-rich minerals by femtosecond laser ablation and solution-nebulization MC-ICP-MS

Journal

ORE GEOLOGY REVIEWS
Volume 81, Issue -, Pages 1271-1286

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.oregeorev.2016.09.028

Keywords

Vanadium; Laser ablation; High resolution MC-ICP-MS; Isotopes; Minerals

Funding

  1. ESI/New-Wave Research

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Vanadium is a redox-sensitive trace metal that occurs in nature as V-II, V-III, and V-V, e.g. in a variety of ore forming minerals like vanadates (hosting V-V), sulfides (e.g., patronite: (VS4)-S-IV?), silicates (e.g., roscoelite, hosting V-III; cavansite, hosting V-IV), and phosphates (e.g., sincosite, hosting V-IV). Similar to other redox-sensitive metals (e.g., Fe, Cu, U), the V isotope compositions of V minerals may provide valuable information for source fingerprinting and redox-controlled processes during ore formation. The first in situ V isotope analyses of several natural V minerals (cavansite, descloizite, patronite, sincosite, vanadinite) were performed in this study employing femtosecond-laser ablation-high resolution-MC-ICP-MS. The delta V-51 values are determined relative to a V metal (Alfa Aesar, 99.5% V) via standard-sample-standard bracketing, and are recast to the Oxford Alfa Aesar solution value. Mass bias was monitored by addition of an Fe standard to the sample aerosol during analyses. For comparison, aliquots of all mineral specimens were analyzed after chromatographic separation by solution-nebulization MC-ICP-MS. Our laser ablation and solution typically data agree well with each other (within 0.1%, units), and indicate a significant variation of delta V-51 values between the analyzed minerals, ranging from 0.5 to + 1.3%. (2 s.e. per analysis typically between 0.04 and 0.06%.). This spread is significantly larger than reported for various reference rocks, and also exceeds the difference for delta V-51 between the bulk silicate Earth and the chondrite average. The extended range of delta V-51 values demonstrates that stable V isotope analyses may provide a new proxy for redox-processes in high- and low-temperature studies, including the fingerprinting of redox-induced V mobilization and enrichment processes during the formation of V-rich ores. (C) 2016 Elsevier B.V. All rights reserved.

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