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This document presents a study on the SHRIMP U–Pb dating and geochemistry of hydrothermal xenotime and monazite from the Huachanggou gold deposit in northern China, providing crucial geochronological constraints on gold mineralization. The findings indicate that the gold mineralization occurred during the Late Triassic, around 210-207 Ma, coinciding with a significant regional compressional event. The research highlights the effectiveness of hydrothermal phosphate U–Pb dating as a tool for understanding com
- Author
- ILHAM ARAZIQ
- Language
- EN