摘要
冷水北沟铅锌矿赋存于元古界栾川群和管道口群地层中,矿体受断裂破碎带及矽卡岩带控制。在系统研究成矿地质条件、地球化学及地球物理综合信息的基础上,归纳并提取了控矿地质因素和物化探找矿标志,从而建立了该矿的地质-地球物理-地球化学找矿模型。
The Lenshuibeigou lead-zinc deposit occurs in Proterozoic Luanchuan group and Guandaokou group formation and is controlled by faulted and fractured zone and skarn zone. Based on a systematic study of the comprehensive information of the related geological conditions for mineralization and the related geochemical and geophysical characteristics, the ore-controlling geological factors and the ore-prospecting guides in geophysical and geochemical exploration were summarized and extracted. As a result, the geological-geophysical-geochemical ore prospecting model for the deposit was constructed.
出处
《金属矿山》
CAS
北大核心
2006年第6期44-47,71,共5页
Metal Mine
基金
教育部科学技术研究重点项目(03178)
教育部跨世纪人才基金项目
国家自然科学基金项目(40172036)
中国地质调查局国土资源调查项目(20023030)
关键词
冷水北沟铅锌矿
找矿信息
找矿模型
Lenshuibeigou lead-zinc deposit, Ore-prospecting information, Ore-prospecting model
