Indication of REEs, Fe, and Mn Composition Typomorphism of Calcite in Metallogenic Fracture Zones with Respect to Local Tectonic Stress Fields: A Case Study of the Qingshan Lead–Zinc Deposit in Northwest Guizhou, China

The Qingshan lead–zinc deposit is one of the typical deposits in the Weining–Shuicheng metallogenic belt in the northwest Guizhou mining area. This deposit is strictly controlled by tectonics, making it highly distinctive. This study used the REE, Fe, and Mn typological characteristics of calcite in the NE mineralization fault zone of the Qingshan lead–zinc deposit in Guizhou to trace the source of ore-forming materials and the local structural stress field characteristics of the fault. Through comprehensively applying structural analysis and LA-ICP-MS technology, the mechanical properties of the fault were analyzed and the REE characteristics of calcite, as well as the variation laws of Fe and Mn, were studied. The results of this study reveal that NE-trending mineralization faults controlled the production of gently inclined ore bodies; the distribution patterns of REEs in the three types of calcite are all “negative Eu-weak negative Ce-right skewed”, with the REE content in calcite near the ore body being significantly increased; furthermore, the variation pattern of Fe and Mn elemental contents in calcite indicate the local stress field characteristics of the ore-forming fault zone. The local opening space of NE-trending compressional and torsional ore-forming faults (where the dip angle slows down) is favorable for the nucleation of mineralized veins. With this study, we therefore improve knowledge regarding the relationships between tectonic stress fields and mineral exploration, serving as a potential source for the prediction of sites that are suitable for the exploitation of tectonic stress fields for mineral exploration, and show that mineral prediction is conducive to achieving the sustainable development of mines.