摘要
大黄花铜多金属矿床位于赤峰金银多金属成矿带南部,通过对物化探异常进行查证和槽探揭露,已圈定了3条矿体,且各矿体均分布于矽卡岩化带中。分析表明:该矿床属于矽卡岩型矿床,以富铜为主,伴生金、银、铅和锌等有益组分;大黄花地区成矿地质条件较好,具有极大的找矿前景。
Dahuanghua Cu polymetallic deposit is located in southern Chifeng Au-Ag polymetallic ore belt. Geophysical and geochemical anomalies and trenching lead to the delineation of 3 ore bodies,all of which are distributed in skarnized rock belt. Analysis show that the deposit belongs to a skarn type deposit with enriched copper as the main mineral that is associated with gold,silver,lead,zinc and so on; Geological conditions are favorable in Dahuanghua Region for mineralization and prospects are great for prospecting.
作者
李伟
刘淼
吴桐
陈井胜
李斌
杨帆
曾宗前
Li Wei Liu Miao Wu Tong Chen Jingsheng Li Bin Yang Fan Zeng Zongqian(Shenyang Center of China Geology Survey Changcheng Drilling Engineering Co.,Ltd.)
出处
《黄金》
CAS
2016年第11期9-12,共4页
Gold
基金
中国地质调查局项目(12120114055501
12120113053400)
关键词
地质特征
矿床成因
大黄花铜多金属矿床
矽卡岩型矿床
geological characteristics
deposit genesis
Dahuanghua Cu polymetallic deposit
skarn type deposit
