Genesis of the Bangbu gold deposit in the southern Tibet: Evidenced from in-situ sulfur isotopes and trace element compositions of pyrite

Earth and Planetary Sciences

• Trace Element 100%
• Sulfur Isotopes 100%
• Tibet 100%
• Greenschist Facies 50%
• Shear Zone 50%
• Arsenopyrite 50%
• Late Triassic 50%
• Quartz Vein 50%
• Remobilization 50%
• Amphibolite Facies 50%
• Zincblende 50%
• Laser Ablation Inductively Coupled Plasma Mass Spectrometry 50%
• Ore-Forming Fluid 50%
• Himalayas 50%
• Boiling 50%
• Gold Mineralization 50%