ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
中祁连东段晋宁期碰撞型花岗岩及其地质意义
  
关键词:eastern central Qilian massif  Neoproterozoic  syn-collisional granite  Jinningian collisional zone  N-S trending structure
基金项目:
作者单位
郭进京 西北大学地质系 
赵凤清 中国地质科学院天津地质矿产研究所 
李怀坤 中国地质科学院天津地质矿产研究所 
摘要点击次数: 8842
全文下载次数: 6841
摘要:
Jinningian Collisional Granite Belt in the Eastern Sector of the Central Qilian Massif and Its Implication
      The Proterozoic granite belt emplaced into the Huangyuan Group a medium-and low-grade metamorphic series of the Proterozoic basement in the eastern central Qilian massif extends in a N S direction.Its geochemical features indicate that it is a syn-collisional S-type granite belt. (917±12) Ma of single-grain zircon U-Pb age constrains its emplacement age. From above it is suggested that the easten central Qilian massif had undergone Jinningian collisional orogenesis. Finally the authors discuss the geological implication of the Proterozoic syn-collisional granite belt in the easten central Qilian massif.
GUO Jin-jing,ZHAO Feng-qing,LI Huai-kun.1999.Jinningian Collisional Granite Belt in the Eastern Sector of the Central Qilian Massif and Its Implication[J].Acta Geoscientica Sinica,20(1):10-15.
查看全文  查看/发表评论  下载PDF阅读器
Copyright©2008 All Rights Reserved
Sponsored by:
Address:: PostCode: Tel: E-mail: