摘要
大厂长坡-铜矿锡多金属矿床规模大,成因十分复杂,对其矿床地质的深入研究,客观地分析其成矿规律,有助于该区进一步的找矿。从赋矿地层、构造、矿体组合、矿物和元素分带几方面分析了长坡—铜坑锡矿床的地质特征,探讨了矿床形成的控制因素,认为地层与构造对矿床的形成起了不同的控制作用,矿床具有层控矿床的特点。
The Changpo-tongkeng tin polymetallic deposit of Dachang is a large scale of deposit with a complicated genesis.Lucubrating the ore mineralogy and analyzing the metallogenic regularity will facilitate further prospecting in the area.The geological character of Changpo-tongkengtin deposit was analyzed from the views of ore bearing strata,structure,orebody combination,mineralogy,and element zoning and the ore contolling factor was discussed.It is believed that strata and structure played different controlling factors to the deposit forming and the deposit shows the characteristics of stratabound deposit.
出处
《矿产与地质》
2004年第5期455-459,共5页
Mineral Resources and Geology
关键词
锡矿床
地质特征
层控性
地层
岩性
构造
长坡-铜坑
广西大厂
tin deposit, geological character, stratabound, statum, lithology, structure, Changpo-tongkeng
