摘要
矿床成矿物质源于斑岩及斑岩期后的岩浆热液,经内生成矿阶段的原生富集作用和表生成矿阶段的富集作用,逐步在相对有利的地质和地球化学环境构造部位富集成矿,属斑岩型中低温外接触带沿层破碎带型原生及氧化Fe-Au多金属矿床。
The metallogenetic material is mainly derived from the porphyry and the postmagmatic thermal fluid,which enriches and forms progressively the ore body in the advantageous geological and geochemical environment by the original and epigenetic enrichment.It belongs to the middle-low T original oxidation Fe-Au multimetallic deposit of porphyry type(bedding fracture zone type).
出处
《云南地质》
2012年第3期301-304,共4页
Yunnan Geology
关键词
金多金属矿
原生及氧化富集
中低温热液型
构造—岩浆控矿
云南鹤庆炉坪
Au Multimetallic Deposit
Original and Oxidation Enrichment
Middle-Low T Hydrothermal Type
Ore Control of Structure-Magma
Luping,Heqing,Yunnan
