Zi-Fu Zhao

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Publications (26)

• Tracing serpentinite recycling through heavy molybdenum isotopes in intraplate basalts
  Geoscience Frontiers 2026 DOI: 10.1016/j.gsf.2026.102420
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• Supplemental Material: Fossil hydrothermal systems theoretically inverted with oxygen isotopes of constituent minerals hydrothermally reequilibrated with internally 18O-enriched fluids: Cooling and mineralizing implications
  2025 DOI: 10.1130/GEOS.S.30128503
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• Supplemental Material: Fossil hydrothermal systems theoretically inverted with oxygen isotopes of constituent minerals hydrothermally reequilibrated with internally 18O-enriched fluids: Cooling and mineralizing implications
  2025 DOI: 10.1130/GEOS.S.30128503.v6
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• Supplemental Material: Fossil hydrothermal systems theoretically inverted with oxygen isotopes of constituent minerals hydrothermally reequilibrated with internally 18O-enriched fluids: Cooling and mineralizing implications
  2025 DOI: 10.1130/GEOS.S.30128503.v4
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• Supplemental Material: Fossil hydrothermal systems theoretically inverted with oxygen isotopes of constituent minerals hydrothermally reequilibrated with internally 18O-enriched fluids: Cooling and mineralizing implications
  2025 DOI: 10.1130/GEOS.S.30128503.v5
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• Supplemental Material: Fossil hydrothermal systems theoretically inverted with oxygen isotopes of constituent minerals hydrothermally reequilibrated with internally 18O-enriched fluids: Cooling and mineralizing implications
  2025 DOI: 10.1130/GEOS.S.30128503.v7
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• Supplemental Material: Fossil hydrothermal systems theoretically inverted with oxygen isotopes of constituent minerals hydrothermally reequilibrated with internally 18O-enriched fluids: Cooling and mineralizing implications
  2025 DOI: 10.1130/GEOS.S.30128503.v2
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• Supplemental Material: Fossil hydrothermal systems theoretically inverted with oxygen isotopes of constituent minerals hydrothermally reequilibrated with internally 18O-enriched fluids: Cooling and mineralizing implications
  2025 DOI: 10.1130/GEOS.S.30128503.v3
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• Supplemental Material: Fossil hydrothermal systems theoretically inverted with oxygen isotopes of constituent minerals hydrothermally reequilibrated with internally 18O-enriched fluids: Cooling and mineralizing implications
  2025 DOI: 10.1130/GEOS.S.30128503.v1
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• Crust‐Mantle Interaction During Continental Deep Subduction: Evidence From Light Mo Isotopes in Post‐Collisional Mafic Igneous Rocks From the East Kunlun Orogen
  Geochemistry, Geophysics, Geosystems 2025 DOI: 10.1029/2025GC012451
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