摘要
在成矿带上主要介绍铜裕沟大型铜矿、日龙沟中型锡矿床的特征。其成因类型均为华力西期海相火山岩型,形成海相火山岩成矿系列。
Middle - sized tin ore bed of to be living into on the mine belt main introduces large copper mine of plentiful channel of copper , middle - sized copper mine of competition what embankment and day Long Gou feature . Such contributing factor form all in the interest of Hua Lixi stage the marine facies volcanic rock moulds , the formation marine facies volcanic rock succeed mine set .
出处
《黄金科学技术》
2006年第3期11-15,共5页
Gold Science and Technology
关键词
成矿带特征
青海省
The one -tenth mine belt feature marine facies volcanic rock intelligence increases -channel Qinghai in copper ravine