摘要
车轱轳沟银多金属矿热液蚀变现象明显,初步确定该矿主要成矿类型为热液充填型银多金属矿床。其中包括贵金属、有色金属及黑色金属是重要的工业原料和我国急需的矿产。本世纪前数十年是我国矿产资源消耗的高峰期,国民经济建设需要的主要金属矿产均不能得到满足。为使社会经济建设顺利进行,提高矿产资源的保障能力,探求矿床(点)存在的地质特征及找矿标志,无疑会对今后的地质找矿工作提供必要的理论与实践需求。
The Chegulugou silver multimodal ores show hydrothermal alternation obviously,they were initially identified that belong to hydrothermal filling Ag polymetallic ore deposits,in metallogenic type,in duding precious metals,and ferrous metals in mineral types which are an important industrial raw materials and much-needed minerals.Decades of beginning of this century is the consumption peak of the national economy can not be met.To enable the smooth socio-economic construction,improve the development of mineral resources,the study of the geological features and prospecting criteria in the mining area can provide the necessary theory and pacific support for the future geological prospecting work.
出处
《吉林地质》
2011年第1期53-56,共4页
Jilin Geology
关键词
车轱轳沟银多金属矿
热液充填
地质特征
找矿标志
Chegulugou silver polymetallic ores
hydrothermal filling
geological features
prospecting criteria