| 刘成维,谷振飞,魏明辉,陈树清,杨云,李玉红.河北相广锰银矿床成矿特征与形成机理[J].矿产勘查,2012,3(2):165-170 |
| 河北相广锰银矿床成矿特征与形成机理 |
| Metallogenic characteristics and formation mechanism of the Xiangguang Mn-Ag ore deposit,Hebei |
| 投稿时间：2011-07-14 |
| DOI： |
| 中文关键词: 锰银矿床 花岗斑岩 成矿特征 河北相广 |
| 英文关键词: Mn-Ag ore deposit metallogenic characteristics formation mechanism Xiangguang,Hebei |
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| 中文摘要: |
| 位于河北省张家口市涿鹿县的相广锰银矿床,是一个较早发现的中型低硫化物型浅成低温热液矿床。矿床赋存于侏罗系后城组和张家口组,与侏罗纪晚期古火山构造关系密切。锰银矿体主要受断裂构造的控制,矿石中矿物组成相当丰富。稀土元素配分形式以及铅同位素组成表明,成矿金属物质主要来自赋矿围岩和下伏地层,同时还有深部物质参与。围岩蚀变特征及蚀变带空间分布特征均显示矿床深部存在高中温热液多金属矿床。 |
| 英文摘要: |
| Located in the Zhuolu county,Zhangjiakou,Hebei Province,North China,the Xiangguang Mn-Ag ore deposit is a middle-scale low-sulfidation epithermal type which was been discovered long time ago. The ore deposit occurs in the Jurassic-age Houcheng and Zhangjiakou Fms.,which is closely related to the paleo-volcanic structural. The Mn-Ag ore mineralization is mainly controlled by a series of shear zones and ore minerals are quite complex. In the light of the REE distribution patterns and Pb isotopic compositions show that the ore-forming materials were derived mainly from country rocks and underlying rocks and partly from deeper sources. The alteration pattern and location of alteration assemblages,which implies that potential exists high or medium-temperature hypothermal deposit at depth. |
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