This analysis reveals genetic linkage between high-temperature mineralization and low-temperature Sb-Au-W deposits, indicating significant U-Pb age constraints.
Table S1. LA-ICP-MS U-Pb dating results and related Tera-Wasserburg U-Pb diagrams of the monitor standards of WX-27 scheelite, KA wolframite, KA cassiterite, Qinghu apatite, 401 apatite, and 44069 monazite. Table S2. LA-ICP-MS U-Pb dating results of multiple hydrothermal minerals (wolframite, cassiterite, apatite, monazite) from the Shaxi, Zhongcun, Zhaixishan, and Niujiaojie W deposits and scheelite from the Zengjiaxi and Zimuchong Sb-W deposit. Table S3. LA-ICP-MS trace element results of scheelite from the Shaxi, Zhongcun, Zhaixishan, and Niujiaojie W deposits and Zengjiaxi and Zimuchong Sb-W deposits.
No takes yet. Share an insight, caveat, or question.
Peng et al. (2025) studied this question.
Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context: