北淮阳成矿带东段东溪低硫型浅成热液金矿床:来自蚀变矿物、流体包裹体和氢氧同位素的证据 |
| 赵丹蕾,倪培,赵子豪,王国光,丁俊英,王波华,方明,郝越进 |
|
The Dongxi low⁃sulfidation type epithermal gold deposit, in the eastern section of the Beihuaiyang metallogenic zone: Evidence from alteration mineralogy, fluid inclusion and H⁃O isotopes |
| Danlei Zhao,Pei Ni,Zihao Zhao,Guoguang Wang,Junying Ding,Bohua Wang,Ming Fang,Yuejin Hao |
| 图5 东溪金矿特征蚀变矿物 (A~C) Miarolitic quartz?adularia in the Dongxi gold deposit,(D~F) typical alteration: carbonatization,silicification and chloritization |
| Fig.5 Photographs of representative samples from the Dongxi gold deposit |
|