• 责任者：Song Chuanzhong (School of Resources and Environment ; Hefei University of Technology ; Hefei 230009 ; China) ; Zhang Hua
• 刊名：Acta Geologica Sinica
• 出版年：2011
• 卷期：85(5)
• 关键词：构造带 ; tectonic zones ; 成矿作用 ; metallogenesis ; 长江中下游成矿带 ; Metallogenic Belt of Middle and Lower Reaches of Yangtze River
• 页码：p.778-788
• 图表：7 illus., 28 refs.
• 分类号：1001
• issnNo：ISSN0001-5717
• isbnNo：CN11-1951/P

The Middle and Lower Reaches of the Yangtze River is a typical area where the tectonic system converted from Mesozoic Tethys tectonic regime to the Pacific tectonic regime. The structural knots of the Middle and Lower Reaches of Yangtze River were the result of tectonic regime transition between Tethys and Pacific tectonic regimes in eastern China,  Dabie Orogenic belt, Tan-Lu Faulting belt, and Middle-Lower Reaches of Yangtze River metallogenic belts directly recorded the transition process of the two tectonic regimes, spatial-temporal relations between deposition-tectonic-magmatic-metallogenic and dynamic setting. Therefore, the intersection positions between various-scale NE-SW trending structural belts and NW-SE trending structural belts are the locations of ore concentration areas and important deposits.