最近关于凤凰山铁矿成因的讨论,有两篇论文先后发表,一是徐熊飞的“关于江苏凤凰山铁矿成因问题的商榷”(刊载于地质论评1959年第5期),一是陈思松的“江苏凤凰山铁矿床成因的初步探讨”(刊载于地质与勘探1958年第23期)。对凤凰山铁矿成因问题,过去一直被认为是中低温热液矿床,列为南山式。在徐熊 Two recent papers on the formation of the Fenghuangshan iron ore mine have been published. First, Xu Xiongfei’s “Discussion on the Causes of the Iron Mines in Fenghuangshan, Jiangsu Province” (published in Geological Review No. 5, 1959) Chen Sisong’s “Preliminary Study on the Genesis of the Fenghuangshan Iron Deposit in Jiangsu Province” (published in Geology and Prospecting, 2358, Issue 23). For the cause of the formation of the Fenghuangshan iron mine, the past has always been considered as a medium- and low-temperature hydrothermal deposit and is classified as Nanshan. In Xu Xiong