摘要
张公岭银金多金属矿床是花岗岩断裂带型中温热液矿床.本文在矿物学研究的基础上,利用热力学原理计算主要金银成矿阶段的物理化学参数,探讨金银运移沉淀机制.在研究中首次采用闪锌矿与银金矿成分地温计.
The Zhanggongling Ag-Au-multimetallic deposit is a granite fault type middle temperature hydrothermal deposit. Based on mineralogy study some physico-chemistry parameters of the main formation stages of Ag-Au-mineralization are calculated. The mechanism of transportation and the precipitation of gold and silver are discussed. The geothermometry based on the composition of electrum and sphalerite is first applied in the study.
出处
《地质找矿论丛》
CAS
CSCD
1993年第1期62-72,共11页
Contributions to Geology and Mineral Resources Research
