• 责任者：Huang Hongwei (State Key Laboratory of Geological Processes and Mineral Resources ; China University of Geosciences ; Wuhan 430074 ; China) ; Du Yuansheng
• 刊名：Geology in China
• 出版年：2009
• 卷期：36(3)
• 关键词：成矿作用 ; metallogenesis ; 盆地演化 ; basin evolution ; 广西 ; Guangxi
• 页码：p.669-676
• 图表：8 illus., 10 refs.
• 分类号：1000
• issnNo：ISSN1000-3657
• isbnNo：CN11-1167/P

The Nandan-Hechi Basin in Guangxi started rifting at the late Early Devonian Emsian stage, and withered and died out gradually with the closure of the paleo-Tethys ocean along the Jinsha River, Honghe River and Majiang River in Triassic. Geological field survey has revealed that crustal movement controlled the formation and evolution of the sedimentary basin, that the basement fault controlled the paleogeographic evolution, and that both of the two factors controlled the lithostratigraphic framework and provided ideal space at the late ore-forming stage. Important mineralization resulted from submarine volcanic exhalation or eruption controlled by the second-order basement fault in the basin.