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西藏某铜多金属矿磁异常特征及解释

邵昌盛 冯永来 谢涛 戴伟 李大虎

成都理工大学学报(自然科学版)Issue(2):231-235,5.
成都理工大学学报(自然科学版)Issue(2):231-235,5.DOI:10.3969/j.issn.1671-9727.2015.02.12

西藏某铜多金属矿磁异常特征及解释

Characteristics and interpretation of magnetic anomalies in a copper deposit of Tibet,China

邵昌盛 1冯永来 1谢涛 1戴伟 2李大虎3

作者信息

  • 1. 四川省核工业地质局 二八二大队,四川 德阳 618000
  • 2. 核工业西藏地质调查院,成都 610081
  • 3. 四川省地震局 工程地震研究院,成都 610041
  • 折叠

摘要

Abstract

In order to determine the distribution and location of the copper deposit,the magnetic anomalies are observed by using ground high-precision magnetic survey method.The occurrence position of ore (mineralized)bodies,the space characteristics of ore-controlling structure,and the characteristics of structure and rock mass can be inferred through analyzing the characteristics of the ground high-precision magnetic survey anomaly and explaining the geological reasons of the magnetic anomaly.Thereby the distribution and location of the copper deposit have been determined.The result is verified by drilling afterwards and is correct.

关键词

高精度磁测/磁异常/铜矿/构造/岩体

Key words

high-precision magnetic survey/magnetic anomaly/copper deposit/structure/rock mass

分类

天文与地球科学

引用本文复制引用

邵昌盛,冯永来,谢涛,戴伟,李大虎..西藏某铜多金属矿磁异常特征及解释[J].成都理工大学学报(自然科学版),2015,(2):231-235,5.

成都理工大学学报(自然科学版)

OA北大核心CSCDCSTPCD

1671-9727

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