摘要
本文在区域地质和矿床地质研究基础上,采用硫同位素、氢氧同位素和流体包裹体等研究,得出黄埠岭金矿为岩浆热液金矿,其产出严格受断裂构造、花岗岩、脉岩河蚀变岩等因素所控制.成矿温度以（160℃～350℃）为主,稳定同位素分析表明硫来源于深部、氢氧同位素特征显示成矿热液来源于岩浆水和大气水混合.
On the basis of regional geology and ore deposit geology, by test studying sulfur isotope, hydrogen oxygen isotope and fluid inclusion. Tthe mineralization genesis of Hangpuling gold deposit is belong to hydrothermal ore band, controlled by structure, granite, dyke, altered rock etc. Mineralization temperature is medium temperature（ 160℃～ 350℃ ）. Analysis of stable isotope, the sulfur is from deep stratum, and magma water and atmospheric water maxed during the ore formation. At last, the Huangpuling gold deposit belongs to medium temperature magma hydrothermal deposit.
出处
《华南地质与矿产》
CAS
2007年第1期33-37,共5页
Geology and Mineral Resources of South China
基金
"山东招远蚕庄金矿黄埠岭矿区深部矿体定位机制及成矿规律研究"部分成果
关键词
黄埠岭金矿
地质特征
成因
山东
Huangpuling gold deposit
geological characteristics
genesis of deposit
Shandong
