摘要
从矿体形态、蚀变、矿化分带、稳定同位素和矿物包裹体等方面论述了矿床与本区岩浆活动在时间、空间和成矿物质来源等方面的关系，提出了银山铜多金属矿床是与燕山早期岩浆活动有关的火山—次火山热液矿床的新认识。
The relationship between the deposit and magma activities in time, space and ore forming material has been discussed based on the research of orebody shape, alteration, mineralization zoning, stable istopes and mineral inclusions etc., and it is believed that the Coppermultimetal ore deposit is a volcanicsubvolcanic hydrothermal deposit related with early yanshannian stage magma activity.
出处
《矿产与地质》
1999年第4期199-203,共5页
Mineral Resources and Geology
关键词
银山
多金属矿床
矿床成因
铜矿床
Yinshan, Coppermultimetal Ore Deposit, Study of Origin
