摘要
新山铁多金属矿矿床规模大、品位高、共(伴)生有铜铅锌银等多种有用组份。经历了火山(海相)喷发、生物化学沉积、成岩作用、地下热水循环改造等多期成矿阶段,属火山喷发沉积—改造(层控碳酸盐)型矿床。
It is a large scale,high grade multimetallic deposit with many paragenetic elements,such as Cu,Pb,Zn,Ag,etc.It has experienced the volcanic eruption（marine facies）,biochemical sedimentation,diagenesis and cyclic reformation of underground thermal fluid,which belongs to the ore deposit of volcanic eruption sedimentation—reformation（stratabound carbonate）type.
出处
《云南地质》
2011年第2期157-159,共3页
Yunnan Geology
关键词
铁铜铅锌银矿
层状脉状残坡积
上三叠统大路边组
浅海碳酸盐沉积
云南勐腊新山
Fe-Cu-Pb-Zn-Ag Deposit
Bedded
Veined
Eluvium-Slope Wash
Upper Triassic Dalubian Formation
Neritic Carbonate Sediment
Xingshan
Mengla
Yunnan
