摘要
通过野外观察和铅、硫、碳同位素测定、稀土元素组成、微量元素和包裹体资料，对该矿床成矿物质的来源作了系统分析，表明金属元素主要来自围岩灯影组，硫具有地层硫与非生物还原硫的混合来源，脉石碳酸盐矿物中的碳来自围岩碳酸盐岩的溶解，重结晶，但混入有有机碳，介质（水）主要来自大气降水。
Through field observation,analyses of compositon of lead, sulphur and carbon isotops,REE, trace elements and inclusiohs, the source of ore-forming material of the Chipu lead-zinc ore deposit is discussed in this paper and have drawn such following conclusions: the ore-forming materials are of polygene. Its metal elements mainly come from wall rock-Dengying Formation;sulphur comes from stratic sulphur and nonbiological reducting sulphur; carbon in the gangue carbonate mineral is formed by the dissolving and recrystallizing of the surounding carbonate rock,but mixed with some organic carbon; medium (watar) mainly comes from precipitation.
出处
《矿物岩石》
CAS
CSCD
1996年第3期54-59,共6页
Mineralogy and Petrology
关键词
成矿物质
铅锌矿床
矿床地质
source of ore-forming material
lead-zinc deposit
Chipu
