Fluid mixing as the dominant ore-forming mechanism in the large Derbur intermediate-sulfidation epithermal deposit: Evidence from in situ O-S isotopes and elemental geochemistry
收藏NIAID Data Ecosystem2026-05-10 收录
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Supplementary material 1. In situ LA -ICP-MS trace element concentrations of sphalerite from the mineralization stage of the Derbur deposit.
Supplementary material 2. In situ LA-MC-ICP-MS sulfur isotope of sphalerite from the mineralization stage of the Derbur deposit.
Supplementary material 3. In situ SIMS oxygen isotope of quartz from the mineralization stage of the Derbur deposit.
创建时间：
2026-01-02
