| 注册
首页|期刊导航|世界有色金属|甘肃敦煌白石滩南金矿地质特征及成因浅析

甘肃敦煌白石滩南金矿地质特征及成因浅析

吴进鹏 曹彦卓

世界有色金属Issue(18):73-75,3.
世界有色金属Issue(18):73-75,3.

甘肃敦煌白石滩南金矿地质特征及成因浅析

Geological Characteristics and Genesis Analysis of Baishitan South Gold Deposit in Dunhuang,Gansu

吴进鹏 1曹彦卓1

作者信息

  • 1. 甘肃省有色金属地质勘查局张掖矿产勘查院,甘肃 张掖 734000
  • 折叠

摘要

Abstract

The Baishitan South Gold Mine in Dunhuang,Gansu Province is mainly distributed at the eastern end of the Tarim Plate,in the western section of the Paleozoic Liuyuan Yujingzi Rift Belt of the Beishan continental margin.During the long history of geological development,it has undergone complex geological structural changes and magmatic activities,and has developed various advantageous mineral types such as cash,copper,tungsten,and iron,demonstrating good mineralization potential.The Baishitan gold deposit is a newly discovered gold deposit in recent years.By analyzing and studying the regional geological background and geological characteristics of the deposit,exploring the genesis of the deposit,it has important indicative and practical significance for searching for similar types of deposits in the region.

关键词

白石滩南金矿/地质特征/矿床成因/甘肃敦煌

Key words

Baishitan South Gold Mine/Geological characteristics/Genesis of mineral deposits/Dunhuang,Gansu

分类

天文与地球科学

引用本文复制引用

吴进鹏,曹彦卓..甘肃敦煌白石滩南金矿地质特征及成因浅析[J].世界有色金属,2023,(18):73-75,3.

世界有色金属

1002-5065

访问量0
|
下载量0
段落导航相关论文