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          <dc:title>Supplemental Material: Dual pathways controlling Mn-carbonate mineralization in redox-stratified basins: Geochemical constraints from the Ortokarnash deposit (Western Kunlun, China)</dc:title>
          <dc:creator>Dao-Hui Pi (25133298)</dc:creator>
          <dc:creator>et al. (281964)</dc:creator>
          <dc:subject>Mineralogy</dc:subject>
          <dc:subject>Ore Deposits</dc:subject>
          <dc:subject>Geochemistry</dc:subject>
          <dc:subject>Economic Geology - Sedimentary</dc:subject>
          <dc:subject>Sedimentary manganese deposit</dc:subject>
          <dc:subject>Ortokarnash deposit</dc:subject>
          <dc:subject>Diagenetic-authigenic dual-pathway model</dc:subject>
          <dc:subject>Redox stratification</dc:subject>
          <dc:subject>Carbon isotopes</dc:subject>
          <dc:description>Table S1: EMPA analysis results of Mn-carbonates from OP-1 and OP-2 profiles (%). Table S2: Major element (%), TOC (%), and C-O isotope (‰) of Mn ores and hosted rocks. Table S3: Rare earth element of Mn ore and hosted rock samples (ppm).&lt;p&gt;&lt;/p&gt;</dc:description>
          <dc:date>2026-09-28T20:25:21Z</dc:date>
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          <dc:identifier>10.1130/GSAB.S.34018437.v1</dc:identifier>
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