摘要
汉德尼(Handeni)金矿是近来在坦桑尼亚绿岩带中发现的大型金矿床。该金矿床产在坦桑尼亚元古宙绿岩带中,矿体位于元古代斜长角闪岩(原岩为基性火山岩)的断裂带中,矿体多呈脉状、似层状,局部网脉状和浸染状,其容矿围岩为石榴石英岩,矿化主要发育黄铁矿化、黄铜矿化、磁黄铁矿化和毒砂化等,金矿物主要为自然金和金银矿,一般颗粒较粗大。研究发现该矿为构造控矿,矿体沿韧性剪切带从北到南呈"S"型分布,且矿体在韧性剪切带的转折端处富集。今后的找矿重点应在Au、Cu、As、Zn等多元素组合高异常部位以及韧性剪切带的转折部位。
The Handeni gold mine is a large gold deposit recently discovered in a Proterozoic greenstone belt in Tanzania. The ore body is located in the fault zone of Proterozoic amphibolite rocks （its protolith is mafic volcanic rocks）. The most ore bodies are of vein- and bedded-looking, and locally of vein network and dissemination forms. The ore-bearing country rock is garnet quartzite. The ore contains pyritization,chalcopyrite, pyrrhotite and arseno- pyrite and so on. Gold minerals are mainly the natural gold and silver,which have generally big grains. Our study found that this ore deposit is controlled by a S-shaped ductile shear zone which extends from north to south. And ore bodies are concentrated at the turning points of the ductile shear zone. The future prospecting direction should focus on the sites with high-anomalies of Au, Cu,As,Zn and other elements as well as the turning loci on the ductile shear zone.
出处
《地质与勘探》
CAS
CSCD
北大核心
2012年第1期177-184,共8页
Geology and Exploration
基金
国外矿产资源风险勘查专项资金(编号:10254B004)资助
