西藏冈底斯中段则莫多拉铜金矿床地质特征及找矿方向

详细信息

收稿日期: 2006-08-21

修回日期: 2006-10-31

刊出日期: 2007-03-31

GEOLOGICAL CHARACTERISTICS AND PROSPECTING GUIDE OF THE ZEMODUOLA COPPER-GOLD DEPOSIT IN CENTRAL GANDISE, TIBET

Received Date: 21 August 2006

Revised Date: 31 October 2006

Publish Date: 31 March 2007

摘要: 则莫多拉铜矿床位于冈底斯中段南缘，矿体主要分布在破碎带中结晶灰岩（大理岩）与火山岩、花岗闪长岩、角闪辉长岩的接触带，土壤地球化学异常测量显示铜、金元素含量较高，具有矿致异常的特征.岩石地球化学测量显示在异常中心存在含矿岩石，矿床地质构造条件较有利，找矿前景良好.
- 地质特征 /
- 则莫多拉 /
- 铜金矿
Abstract: The Zemoduola copper-gold deposit is located in central Gandise, Tibet, with ore bodies occurring in the fracture zones within the contact of crystalline limestone and volcanic rocks, granodiorite or bojite. Soil geochemical survey shows high Cu and Au abnormalities led by mineralization. Lithogeochemical survey suggests that ore-bearing rocks exist in the abnormality center. The deposit is in a favorable structural background, with great exploring potential.
- geological characteristics /
- Zemoduola /
- copper-gold deposit