| 王世平,原淑军,刘春香.招掖地区上庄金矿床地质特征及矿体分布规律[J].地质找矿论丛,1998,(2):67-75 |
| 招掖地区上庄金矿床地质特征及矿体分布规律 |
| GEOLOGICAL CHARACTERISTICS AND ORE BODY DISTRIBUTION OF SHANGZHUANG AU DEPOSIT,ZHAOYE DISTRICT,SHANDONG PROVINCE |
| 投稿时间：1997-10-27 修订日期：1998-03-23 |
| DOI：10.6053/j.issn.1001-1412.1998.2. 008 |
| 中文关键词: 上庄岩体 上庄-望儿山断裂 矿体 分布规律 |
| 英文关键词:Shangzhuang granite Shangzhuan wangershan fault ore body distribution pattern |
| 基金项目: |
|
| 摘要点击次数: 1203 |
| 全文下载次数: 1521 |
| 中文摘要: |
| 上庄金矿床是胶东招掖地区焦新矿田中一处大型金矿床,受焦家断裂的分支断裂---上庄 望儿山断裂控制,产在郭家岭型花岗岩上庄岩体与玲珑花岗岩的接触带上。本文介绍了矿床的主要地质特征,分析了控矿断裂的性质及控矿规律,论述了上庄岩体的特征及其形成年代,最后阐明了矿体分布规律,对指导找矿有一定的参考意义。 |
| 英文摘要: |
| Shangzhuang Au deposit is a large size deposit located in Jiaojia Xincheng Au ore field,zhao Ye district.It is controled by shangzhuang Wangershan fault,a secondery fault of Jiaojia fault occurring at the contact between shangzhuange granit (Guoialing type granite)and Linglong granite.In this paper is described geological characteristics of the Au deposit and the graites,annlysed property of the fault and ore controling factors and significance to future exploration in the district. |
| 查看全文 查看/发表评论 下载PDF阅读器 |
| 关闭 |
|
|
|
