首页 | 本学科首页   官方微博 | 高级检索  
     

秘鲁南部深大断裂与古新世斑岩铜矿带地质特征
引用本文:张杨,高光明,席振,李建华.秘鲁南部深大断裂与古新世斑岩铜矿带地质特征[J].南方金属,2011(2).
作者姓名:张杨  高光明  席振  李建华
作者单位:中南大学,地球科学与信息物理学院,湖南,长沙,410083
摘    要:秘鲁南部古新世斑岩铜矿带是全球最重要的智利-秘鲁矿集区的一部分,紧邻印加断层两旁密集分布着许多斑岩铜矿床(矿点).本文通过收集和整理相关文献以及实地考察,总结了该带深大断裂系统的地质特征,斑岩矿床的地质特征,并进一步分析深大断裂系统与斑岩矿床的关系.对认识该区的构造活动以及找矿实践具有指导意义.

关 键 词:秘鲁  深大断裂  斑岩铜矿  板块  印加断层  遥感  构造  

Geological features of the deep fracture systems and the Paleocene Cu-porphyry belt in southern Peru
ZHANG Yang,GAO Guang-ming,XI Zhen,LI Jian-hua.Geological features of the deep fracture systems and the Paleocene Cu-porphyry belt in southern Peru[J].Southern Metals,2011(2).
Authors:ZHANG Yang  GAO Guang-ming  XI Zhen  LI Jian-hua
Affiliation:ZHANG Yang,GAO Guang-ming,XI Zhen,LI Jian-hua(School of Geosciences and Info-Physics,Central South University,Changsha 410083,Hunan)
Abstract:The Paleocene Cu-Porphyry Belt located in Southern Peru is a part of the Chile-Peru ore-concentrated area that is the most important Cu-Porphyry belt in the world,and there are a plenty of Cu-porphyry deposits along the Incapuquio faults system.By gathering relevant information and conducting field survey,the geological features of the deep fracture systems and the Paleocene Cu-Porphyry belt in Southern Peru were summarized,and the relationship between the deep fracture and the Cu-porphyry was explored.The ...
Keywords:Peru  deep fracture  porphyry copper  plate tectonics  Incapuquio faults system  remote sensing  tectonic  
本文献已被 CNKI 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号