摘要
上别列铜多金属矿床属水泄咱咧铜钴矿区外围新发现的矿点，赋存于兰坪-思茅盆地中生带红色碎屑岩建造厂街-水泄成矿带中，区内有30余处矿点，中-小型铜、铁矿点二处。认为属改造型中低温热卤水裂隙充填矿床，水泄咱咧铜钴矿区外围具备进一步找矿的条件。
The Shangbielie Cu muhimetallic deposit is a new ore occurrence discovered outside the Shuixie- Zanlie Cu- Co orefield, which exists in Changjie- Shuixie metallogenetic Zone of Mesozoic red clastic rock formation in Lanping - Simao basin. We believe that this ore deposit belongs to the middle - low T thermal brine fissure filling ore deposit of reformation type. The area a- round Shuixie - Zanlie Cu - Co orefield has the condition of further ore - prospecting.
出处
《云南地质》
2008年第2期203-209,共7页
Yunnan Geology
关键词
铜多金属
中低温热卤水
裂隙充填矿床
后期改造
水泄上别咧云南
Cu Multimetallic Deposit
Middle -Low T Thermal Brine
Fissure Filling De- posit
Reformation Type
Shangbielie, Shuixie, Yunnan
