| 李兆麟,杨忠芳.广东莲花山钨矿成矿机制探讨[J].地质找矿论丛,1992,(1):63-70 |
| 广东莲花山钨矿成矿机制探讨 |
| A STUY ON GENESIS OF LIANHUASHAN TUNGSTEN DEPOSIT, GUANGDONG PROVINCE |
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| DOI：10.6053/j.issn.1001-1412.1992.1. 006 |
| 中文关键词: 莲花山钨矿 包裹体 粒间溶液 |
| 英文关键词: |
| 基金项目:国家自然科学基金 |
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| 中文摘要: |
| 通过对广东莲花山钨矿石英包裹体成矿温度测定、成矿溶液化学成分以及氧、硫同位素组成特征研究表明,莲花山钨矿是一个与石英斑岩有关的中高温热液矿床,成矿流体来自岩体中的粒间溶液,晚期有部分天水混入. |
| 英文摘要: |
| The microthermometric analyses of quartz fluid inclusions, chemical composition and δ18O、δ34S evolution regularity of ore-forming fluid in tungsten quartz vein indicate that Lian Hua Shan tungsten deposit belongs to mesothermal-hypothermal deposit related to quartz porphyry. Various ore hodies have similar physicochemical conditions. The ore-forming fluid derived from the intergrain fluid which mixed with meteoric water. |
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