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.
The microthermometric analyses of quartz fluid inclusions, chemical composition and δ^(18)O、δ^(34)S 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.
出处
《地质找矿论丛》
CAS
CSCD
1992年第1期63-70,共8页
Contributions to Geology and Mineral Resources Research
基金
国家自然科学基金
