摘要
铅锌矿位于兰坪盆地铅锌银铜多金属矿集区,上三叠统灰岩为主要赋矿地层,铅质源自海底火山喷发,属火山-沉积改造型中低温热液矿床。
This ore deposit is in the concentration area of Pb - Zn - Ag - Cu muhimetallic deposits in Lanping basin. The main ore - bearing bed is Upper Triassic limestone. The Pb is originated from the submarine volcanic eruption, which belongs to the volcanic - sedimentary reformation middle -low T hydrothermal deposit.
出处
《云南地质》
2009年第3期280-284,共5页
Yunnan Geology
关键词
中低温铅锌矿
沉积改造
上三叠统层控
灰岩破碎带
云南兰坪青甸湾
Middle - Low T Pb - Zn Deposit
Sedimentary Reformation
Upper Triassic Stratabound
Limestone Fracture
Qingdianwan, Lanping, Yunnan
