• 责任者：Qiu Junting (School of Earth Sciences and Resources ; China University of Geosciences ; Beijing 100083 ; China) ; Yu Xinqi
• 刊名：Earth Science Frontiers
• 出版年：2011
• 卷期：18(5)
• 关键词：钼矿 ; molybdenum ores ; 铅锌矿床 ; lead-zinc deposit ; 推覆构造 ; nappe structure ; 武夷山 ; Wuyi Mountains
• 页码：p.243-255
• 图表：6 illus., 2 tables, 30 refs.
• 分类号：1001
• issnNo：ISSN1005-2321
• isbnNo：CN11-3370/P

The nappe structures in Huangbi mining district, North Wuyi Mountains, Southeast China are NNE oriented with dip angles towards WNW. It was found in field investigation that the nappe structures destroyed the previous Mo deposit on one hand, while their secondary fissures obviously controlled the distribution of later Pb-Zn deposit. According to SHRIMP U-Pb zircon, Re-Os and ³⁹Ar-⁴⁰Ar dating results, this paper reports the order of the tectonics-magmatism-mineralization processes in Huangbi district.