• 责任者：Liang Lei (Guilin Research Institute of Geology for Mineral Resources ; Guilin 541004 ; China) ; Yan Zigei
• 刊名：Mineral Resources and Geology
• 出版年：2011
• 卷期：25(5)
• 关键词：金矿 ; gold ores ; 银矿 ; silver ores ; 变质核杂岩 ; metamorphic core complexes ; 广西 ; Guangxi Province
• 页码：p.353-359
• 图表：4 illus., 6 refs.
• 分类号：1001
• 出版序号：437
• issnNo：ISSN1001-5663
• isbnNo：CN45-1174/TD

The gold-silver ores in Shiwo area are structure-controlled alteration-type deposits. Their mineralizations are related to the metamorphic core complex characterized by denudational fault belt in basement rock. The gold-silver ores mainly occur in the range of denudational fault belt, forming the specific ore forming-layer effect. The mineralization is also related to the Yanshanian magmatic activity, which provided accommodate structures mainly consist of fragile faults and shear zone and most part of hydrothermal fluids for the formation of the deposits.