Supplemental Material: Vanished evaporites, halokinetic structure, and Zn-Pb mineralization in the world-class Angouran deposit, northwestern Iran
Figure S1: (A) Raman spectra of anhydrite and dolomite inclusions in S1 sphalerite. (B) Raman spectra of dolomite and spherical calcite inclusions in double-terminated quartz. (C) Raman spectra of tabular dolomite inclusion and the host double-terminated quartz. Figure S2: Concentrations of Li, Na, and K versus Al of the double-terminated quartz at Angouran. Table S1: U-Pb data of zircons from Miocene tuffaceous pyroclastic rocks and volcanic clasts-bearing breccias in the Angouran deposit. Table S2: Sulfur isotope composition of sulfides in the Angouran deposit. Table S3: Quantitative LA-ICP-MS trace element data of double-terminated quartz in the Angouran deposit (concentrations in ppm). Table S4: Oxygen isotope composition of quartz from the sulfide ores and footwall schist in the Angouran deposit.