• 责任者：Zhou Taofa (School of Resources and Environmental Engineering ; Hefei University of Technology ; Hefei 230009 ; China) ; Fan Yu
• 刊名：Acta Geologica Sinica
• 出版年：2011
• 卷期：85(5)
• 关键词：成矿作用 ; metallogenesis ; 成岩作用 ; diagenesis ; 长江中下游成矿带 ; Metallogenic Belt of Middle and Lower Reaches of Yangtze River
• 页码：p.712-730
• 图表：12 illus., 1 table, 56 refs.
• 分类号：1001
• issnNo：ISSN0001-5717
• isbnNo：CN11-1951/P

The Middle-Lower Yangtze River valley is one of the most important Cu-Fe polymetallic belts in China, in which hosts many volcanic basins, such as Li-Shu, Li-Yang, Ning-Wu, Fan-Chang, Lu-Zong, Huai-Ning and Jin-Niu volcanic basin. Based on the contributions of the previous researchers as well as the fundamental studies in recent years mainly on Luzong Basin and Ningwu Basin, this paper discussed the geological characteristics, the temporal-spatial framework, and geochemistry, geochronology of petrogenesis and mineralization and metallogenetic model of the volcanic basins in the Middle-Lower Yangtze metallogenetic belt. The chronological results of the igneous rocks suggest that the magmatic rocks in the volcanic basins formed in Early Cretaceous (135~123 Ma). This paper proposes a petrogenetic and metallogenetic model for the volcanic basins in the Middle and Lower Yangtze metallogenetic belt.