• 责任者：Hu Yunhu (College of Earth Sciences ; Guilin University of Technology ; Guilin 541004 ; China) ; Luo Hongbo
• 刊名：Mineral Resources and Geology
• 出版年：2012
• 卷期：26(1)
• 关键词：银矿 ; silver ores ; 锑矿 ; antimony ores ; 成矿规律 ; metallogenic regularity ; 广西 ; Guangxi
• 页码：p.40-44
• 图表：2 illus., 2 tables, 8 refs.
• 分类号：1001
• issnNo：ISSN1001-5663
• isbnNo：CN45-1174/TD

Zhenlongshan fornix is located at the junction position of the Binyang, Hengxian, Guigang counties, Guangxi. Mineralization belts of Ag, Cu, Pb, Zn, Sb, As, Au is mass distributed along the two deep faults of northern and southern part but less in the outer settlement zone of the fornix. The mineralization is controlled by the stratum construction, tectonic activity and magma activity. Strata provided some metallogenic material sources for mineralization and carbon-containing construction played a role in activating the metallogenic elements of strata. Tectonic activities prompted the stratiagraphic occurrence of dynamic metamorphism, controlled magmatic intrusion and deposits (mineralization) distribution. Magma activities for mineralization bring a lot of metallogenic material and controlled the mineralization type of the fornix area.