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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Wayne R. Premo</dc:contributor>
  <dc:contributor>Nikolay N. Mel’nikov</dc:contributor>
  <dc:contributor>Poul Emsbo</dc:contributor>
  <dc:creator>Leonid A. Neymark</dc:creator>
  <dc:date>2014</dc:date>
  <dc:description>We present strontium isotopic (&lt;sup&gt;88&lt;/sup&gt;Sr/&lt;sup&gt;86&lt;/sup&gt;Sr and &lt;sup&gt;87&lt;/sup&gt;Sr/&lt;sup&gt;86&lt;/sup&gt;Sr) results obtained by &lt;sup&gt;87&lt;/sup&gt;Sr–&lt;sup&gt;84&lt;/sup&gt;Sr double spike thermal ionization mass-spectrometry (DS-TIMS) for several standards as well as natural water samples and mineral samples of abiogenic and biogenic origin. The detailed data reduction algorithm and a user-friendly Sr-specific stand-alone computer program used for the spike calibration and the data reduction are also presented. Accuracy and precision of our δ&lt;sup&gt;88&lt;/sup&gt;Sr measurements, calculated as permil (‰) deviations from the NIST SRM-987 standard, were evaluated by analyzing the NASS-6 seawater standard, which yielded δ&lt;sup&gt;88&lt;/sup&gt;Sr = 0.378 ± 0.009‰. The first DS-TIMS data for the NIST SRM-607 potassium feldspar standard and for several US Geological Survey carbonate, phosphate, and silicate standards (EN-1, MAPS-4, MAPS-5, G-3, BCR-2, and BHVO-2) are also reported. Data obtained during this work for Sr-bearing solids and natural waters show a range of δ&lt;sup&gt;88&lt;/sup&gt;Sr values of about 2.4‰, the widest observed so far in terrestrial materials. This range is easily resolvable analytically because the demonstrated external error (±SD, standard deviation) for measured δ&lt;sup&gt;88&lt;/sup&gt;Sr values is typically ≤0.02‰. It is shown that the “true” &lt;sup&gt;87&lt;/sup&gt;Sr/&lt;sup&gt;86&lt;/sup&gt;Sr value obtained by the DS-TIMS or any other external normalization method combines radiogenic and mass-dependent mass-fractionation effects, which cannot be separated. Therefore, the “true” &lt;sup&gt;87&lt;/sup&gt;Sr/&lt;sup&gt;86&lt;/sup&gt;Sr and the δ&lt;sup&gt;87&lt;/sup&gt;Sr parameter derived from it are not useful isotope tracers. Data presented in this paper for a wide range of naturally occurring sample types demonstrate the potential of the δ&lt;sup&gt;88&lt;/sup&gt;Sr isotope tracer in combination with the traditional radiogenic &lt;sup&gt;87&lt;/sup&gt;Sr/&lt;sup&gt;86&lt;/sup&gt;Sr tracer for studying a variety of biological, hydrological, and geological processes.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1039/C3JA50310K</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Royal Society of Chemistry</dc:publisher>
  <dc:title>Precise determination of δ&lt;sup&gt;88&lt;/sup&gt;Sr in rocks, minerals, and waters by double-spike TIMS: A powerful tool in the study of chemical, geologic, hydrologic and biologic processes</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>