• 责任者：Xu Qiang (East China Geological Exploration Bureau of Nonferrous Metals in Jiangsu Province ; Nanjing 210007 ; China) ; Xue Weichong
• 刊名：Journal of Geology
• 出版年：2013
• 卷期：37(4)
• 页码：p.647-652
• issnNo：ISSN1674-3636
• isbnNo：CN32-1796/P

Tieshan lead-zinc deposit was located in Zhenghe County which was in the east of Fujian Province, and was in Mesozoic- Cenozoic volcanic active zones. Tectonics was on the junction of Jian＇ou-Suichang ancient anteklise and coastal subsidence of Zhejiang and Fujian. The ore bodies were occurred in the contact zones of Daoxiang Formation of upper Sinian to early Paleozoic and along the bedding fissures on the country rocks in the contact zones of Tieshan contaminated syenite and maple biotite granite in late Yanshanian. The occurrence of the ore bodies and contact zones were almost the same and mainly controlled by stratigraphic occurrence and the con- tact zones. The shapes of ore bodies were of stratiform, lens and veins. The ore grade was high and was mainly lead-zinc and then brass lead-zinc and lead-zinc magnetite. The deposit materials were from the strata and rock especially the volcanic interlayers in the sediment rocks. It was of strata bound skarn type deposit.