摘要
玛瑙山铁锰多金属矿床产于棋梓桥组底部层位中，矿体呈似层状。除铁、锰、铅外，伴生有银、铟。由泥盆纪沉积期成岩成矿作用和燕山期岩浆热液叠加成矿作用所形成的沉积改造—岩浆热液叠加型铁锰多金属矿床。
Manaoshan Fe Mn polymetallic ore deposit occurs in the bottom of Qiziqiao formation.The orebody looks beded.Iron,manganese and lead are the major minerals,accompanying silver and indium.Its forming experienced two stages,the first stage is diagenetic mineralization in Devonian and the second stage is magmatic hydrothermal superimposed miner alization in Yanshaian.
出处
《湖南地质》
1997年第3期163-166,共4页
Hunan Geology
基金
湖南地质矿产局地质勘查项目
