| 张乐凯.张公岭银金多金属矿床成矿物理化学条件[J].地质找矿论丛,1993,(1):62-72 |
| 张公岭银金多金属矿床成矿物理化学条件 |
| STUDY ON THE FORMATION PHYSICO-CHEMICAL CONDITION OF ZHANGGONGLING AU-AG-MULTIMETAL DEPOSIT |
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| DOI：10.6053/j.issn.1001-1412.1993.1. 006 |
| 中文关键词: 矿物地温计 地质热力学 金银矿床 广西 |
| 英文关键词: |
| 基金项目: |
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| 中文摘要: |
| 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。 |
| 英文摘要: |
| 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. |
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