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云南会泽麒麟厂铅锌矿床构造地球化学及定位预测
韩润生; 陈进
2001
Source Publication矿物学报
ISSN1000-4734
Volume21Issue:4Pages:667-673
Abstract在论述断裂构造地球化学基本理论与方法的基础上,深入讨论了会泽麒麟厂铅锌矿床断裂构造地球化学特点,认为断裂构造地球化学异常集中区是进行隐伏矿定位预测的重要依据,提出了1571中段44-62剖面线间的深部等重点定位找矿靶区,已被验证工程证实,发现八号隐伏矿体。该方法对隐伏矿定位预测和评价具有重要指导意义。
metadata_83中国科学院地球化学研究所
Keyword铅锌矿床 构造地球化学 隐伏矿定位预测 地质工程验证 云南 找矿靶区
Indexed ByCSCD
Language中文
CSCD IDCSCD:690686
Citation statistics
Cited Times:22[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/2599
Collection环境地球化学国家重点实验室_环境地球化学国家重点实验室_期刊论文
Recommended Citation
GB/T 7714
韩润生,陈进. 云南会泽麒麟厂铅锌矿床构造地球化学及定位预测[J]. 矿物学报,2001,21(4):667-673.
APA 韩润生,&陈进.(2001).云南会泽麒麟厂铅锌矿床构造地球化学及定位预测.矿物学报,21(4),667-673.
MLA 韩润生,et al."云南会泽麒麟厂铅锌矿床构造地球化学及定位预测".矿物学报 21.4(2001):667-673.
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