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    <responseDate>2026-10-10T19:08:15Z</responseDate>
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    <identifier>10.57760/sciencedb.34501</identifier>
    <datestamp>2026-07-09T10:48:04Z</datestamp>
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  <dc:date>2026-07-09</dc:date>
  <dc:title>Provenance data of the MLB section in South China</dc:title>
  <dc:identifier>doi:10.57760/sciencedb.34501</dc:identifier>
  <dc:language>en</dc:language>
  <dc:description>Five sandstone samples from the MLB section were selected for heavy mineral assemblage analysis. Geochronological and geochemical analyses were performed on three samples at heights of 0 m, 71.8 m, and 129 m (Fig. 1c). For zircon U&amp;ndash;Pb ages, 206Pb/238U ages are used for grains younger than 1000 Ma, whereas 207Pb/206Pb ages are used for older grains. In addition, zircon ages with concordance values lower than 90% are excluded.</dc:description>
  <dc:subject>South China;  Late Paleozoic; Detrital zircon;  Provenance</dc:subject>
  <dc:creator>GAO Biao</dc:creator>
  <dc:rights>PUBLIC</dc:rights>
  <dc:rights>https://creativecommons.org/licenses/by-nc/4.0/</dc:rights>
  <dc:type>dataset</dc:type>
  <dc:publisher>Science Data Bank</dc:publisher>
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