摘要
陈家杖子金矿是通过1∶5万化探工作发现的斑岩型金多金属矿,其地球化学异常特征可作为在该区寻找类似矿床标志。该矿东部还有形成多金属矿的潜力。在此类土壤覆盖区应采用土壤测量。该金矿的发现反映了在我国中西部地区利用常规方法来发现新矿床的巨大潜力。
The Chenjiazhangzi gold deposit is a porphyry gold polymetallie deposit discovered by 1： 50000 geochemical exploration. The characteristics of its geochemical anomaly can be used as indicators in search for similar deposits in this area. The eastern part of the ore district might still have concealed polymetallic deposits. Soil survey should be adopted in such soil overburden areas. The discovery of this gold deposit demonstrates the great potential of the traditional methods in finding new deposits in central and western China.
出处
《物探与化探》
CAS
CSCD
2005年第4期308-311,315,共5页
Geophysical and Geochemical Exploration
关键词
陈家杖子金矿
金多金属矿
地球化学特征
土壤测量
Chenjiazhangzi gold deposit
gold polymetallic deposit
geochemical characteristics
soil survey
