@article{20160628094849-495162,
 author={{OK10a-b}},
 title={Aliquot at \nolinkurl{/}},
 journal={\href{http://dream.misasa.okayama-u.ac.jp/?q=20160628094849-495162}{DREAM}},
 volume={20},
 pages={20160628094849-495162},
 year={2016},
 url={http://dream.misasa.okayama-u.ac.jp/?q=20160628094849-495162},
}

<?xml version="1.0" encoding="UTF-8"?>
<acquisitions>
  <acquisition>
    <global_id>20130413183551-399810</global_id>
    <name>LF4907</name>
    <device>Thermo Scientific MAT253</device>
    <technique>IRMS with LF</technique>
    <operator></operator>
    <sample_global_id>20160628094849-495162</sample_global_id>
    <sample_name>OK10a-b</sample_name>
    <description>Accounting a difference of Δ(17O/16O) for meteoric water from ones for the silicate/oxide minerals (Tanaka and Nakamura, 2013), δ(17O/16O)_VSMOW value of silicate/oxide minerals, in the strict sense, is calculated as, δ(17O/16O)_VSMOW = δ(17O/16O) – 0.034, where a relationship between the δ(17O/16O)_VSMOW and the terrestrial silicate fractionation line is expressed as Δ(17O/16O)_TSFL = [ln{(δ(17O/16O)_VSMOW + 0.034) / 1000 + 1} – 0.527 × ln(δ(18O/16O) / 1000 + 1)] / 1000, based on the measurements of VSMOW2 and San Carlos olivine standard (δ18O/16O = 5.27±0.12, δ17O/16O_VSMOW = 2.71±0.07).</description>
    <chemistries>
      <analysis>
        <nickname>d17O</nickname>
        <value>3.827</value>
        <unit>permil</unit>
        <uncertainty>0.026</uncertainty>
        <label></label>
        <info></info>
      </analysis>
      <analysis>
        <nickname>d18O</nickname>
        <value>4.973</value>
        <unit>permil</unit>
        <uncertainty>0.008</uncertainty>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>D17O</nickname>
        <value>1.239</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
</acquisitions>