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云南会泽铅锌矿床构造控矿规律及其隐伏矿预测
韩润生; 陈进
2001
Source Publication矿物学报
ISSN1000-4734
Volume21Issue:2Pages:265-269
Abstract本文对会泽铅锌矿成矿构造体系、构造控矿型式进行研究,认为小江深断裂带和曲靖-昭通隐伏断裂带为矿床形成提供了有利的构造背景,矿床严格受北东向压扭性断裂控制,“阶梯状”和“多字型”构造是矿区具有普遍性的控矿构造型式,北东构造带是主要的成矿构造体系,提出麒麟厂矿床主矿体向南西向侧伏,通过工程验证新增铅锌矿金属储量近100万吨。
metadata_83中国科学院地球化学研究所
Keyword构造控矿规律 隐伏矿 定位预测 “多字形”构造型式 铅锌矿床 云南 矿床地质 成矿构造体系
Indexed ByCSCD
Language中文
CSCD IDCSCD:690598
Citation statistics
Cited Times:25[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/2601
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. 云南会泽铅锌矿床构造控矿规律及其隐伏矿预测[J]. 矿物学报,2001,21(2):265-269.
APA 韩润生,&陈进.(2001).云南会泽铅锌矿床构造控矿规律及其隐伏矿预测.矿物学报,21(2),265-269.
MLA 韩润生,et al."云南会泽铅锌矿床构造控矿规律及其隐伏矿预测".矿物学报 21.2(2001):265-269.
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