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Magmatic-Hydrothermal Superlarge Metallogenic Systems A Case Study of the Nannihu Ore Field |
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| Authors: | Wang Changming Cheng Qiuming Zhang Shouting Deng Jun Xie Shuyun |
| Institution: | 1. State Key Laboratory of Geological Processes and Mineral Resources, Key Laboratory of Lithosphere Tectonics and Lithoprobing Technology of Ministry of Education, China University of Geosciences, Beijing 100083, China;Department of Earth and Space Science and Engineering, York University, Toronto ON M3J1P3, Canada 2. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences,Beijing 100083, China; Department of Earth and Space Science and Engineering, York University,Toronto ON M3J1P3, Canada 3. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences,Beijing 100083, China 4. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences,Wuhan 430074, China; Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China;Department of Earth and Space Science and Engineering, York University, Toronto ON M3J1P3, Canada |
| Abstract: | Located in the Qinling molybdenum metallogenic belt on the southern margin of North China craton, the Nannihu molybdenum (-tungsten) ore field, consisting of the Nannihu, Sandaozhuang, and Shangfang deposits, represents a superlarge skarn-porphyry molybdenum (-tungsten) accumulation. Outside the ore field, there are some hydrothermal lead-zinc-silver deposits found in recent years, for example, the Lengshuibeigou, Yindonggou, Yangshuwa, and Yinhegou deposits. Ore-forming fluid geochemistry indicates that these deposits belong to the same metallogenic system. The hydrothermal solutions were mainly derived from primary magmatic water in the early stage and from the mixture of the primary magmatic water and meteoric water in the later stage, with an obvious decreasing tendency in temperature, salinity and gas-liquid ratio of fluid inclusions. Sulfur and lead isotope data show that the ore-forming substances and related porphyries were mainly derived from the lower crust, and a hidden magmatic chamber is indicated by aeromagnetic anomaly and drill hole data indicate that the Nannihu granite body extends to being larger and larger with depth increasing. The large-scale mineralization was the consequence of lithospheric extension during the late stage of the tectonic regime when the main compressional stress changed from NS-trending to EW-trending. |
| Keywords: | magmatic-kydrothermal metallogenic system superlarge deposit ore-forming fluid dynamic process nannihu ore field |
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