| 陈仁义,刘海光,马文义.新疆琼河坝铜金矿化地质特征及成因机理[J].地质与勘探,1995,(1): |
| 新疆琼河坝铜金矿化地质特征及成因机理 |
| Geological Characteristics and Genetic Mechanism of Cu-Au Mineralization in Qiongheba,Xinjiang |
| |
| DOI： |
| 中文关键词: 铜金矿化，夕卡岩，斑岩，剥蚀程度，琼河坝 |
| 英文关键词: Cu-Au mineralization,skarn,porphyry,the depth of denudation,Qiongheba, |
| 基金项目: |
| 陈仁义 刘海光 马文义 |
| 中国地质大学，中国地质科学院矿床所，新疆第二区调大队 |
| 摘要点击次数: 2960 |
| 全文下载次数: 1458 |
| 中文摘要: |
| 通过研究琼河坝地区的含矿岩系、铜金矿化、流体包裹体和氢氧同位素，认为２０２铜矿为斑岩型矿床，绿石沟铜矿为夕卡岩型矿床，剥蚀程度是本区铜金找矿的关键。 |
| 英文摘要: |
| After studying ore-bearing rock series,Cu-Au Mineralization,fluid inclusion and H-O isotopes,it is believed that 202 Cu deposit is a porphyry one,and that Lushigou Cu deposit is a skarn.Then,it is pointed out that the key to prospecting Cu and Au in studied area is the depth of denudation. |
|
查看全文
查看/发表评论 下载PDF阅读器 |
| 关闭 |
|
|
|
