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1.Large quantities of analyses and statistics of gold abundance in different strata and locks combined with lead isotope data suggest that greenstone of Late Archean Xigudui Formation is the source bed of gold deposits.
通过铅、硫、氢、氧同位素以及不同层位、岩石金丰度的大量统计,成矿与构造、岩浆岩关系研究,表明金的成矿作用具有多来源、多成因、多阶段的特点,金矿有明显的层控性,晚太古代西?囟炎槁萄沂墙鸬目笤床恪 区域东西向复式背斜和南北向韧性剪切带分别控制了成矿区和矿田、矿床、矿体的分布。收藏指正
2.STABLE ISOTOPE AND TRACE ELEMENT STUDIES ON THE HEMLO GOLD DEPOSIT, ONTARIO, CANADA
加拿大安大略省赫姆洛金矿的稳定同位素和痕量元素研究收藏指正
3.HYDROGEN AND OXYGEN ISOTOPE COMPOSITIONS AND MINERALIZATION OF THE ZHANGJIAKOU GOLD DEPOSITS, HEBEI PROVINCE
河北张家口金矿床氢、氧同位素组成与矿床成因收藏指正
4.LEAD ISOTOPE COMPOSITION OF GOLD DEPOSITS, NORTH-WESTERN JIAODONG SHANDONG, AND ITS GEOLOGICAL SIGNIFICANCE
胶东西北部地区金矿床铅同位素特征及其地质意义收藏指正
5.Sulfur and Lead Isotope Geochemistry of the Orogenic Gold Deposits in East Kunlun Area,Qinghai Province
青海东昆仑造山型金矿硫、铅同位素地球化学收藏指正
6.According to the comparison and analysis of mineral composition and geochemical characteristics of trace element, sulfur isotope, hydrogen and oxygen isotope, lead isotope and rare earth element in the gold ore and the altered spilite from the deposits of Huachanggou Gold Mine, it was confirmed that the gold ore had obvious succession of the basic igneous rock.
摘要通过对铧厂沟金矿床金矿石和蚀变细碧岩矿物组成、微量元素、硫同位素、氢氧同位素、铅同位素及稀土元素地球化学特征地对比分析，得出金矿石对该基性火山岩存在明显的继承性。收藏指正
7.The sulfur isotope composition of the gold ores is within the range of 5.3‰～9.4‰ δ 34S_ V-CDT.
矿石硫同位素组成稳定,δ34SV_CDT变化范围为5.3‰～9.4‰。收藏指正
8.In this paper,the authors indroduced in detail the characteristics of the isotope constitutions of the gold-bearing quartz veins,the metamorphics of the Archaean Taihua Group and relative vein rocks in the Xiaoqinling gold field,and discussed the sulfur source in veins.
本文系统地介绍了小秦岭金矿田内含金石英脉,太古界太华群变质岩和有关脉岩的硫同位素特征,并对矿脉中硫的来源作了探讨。收藏指正
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