ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
巴颜喀拉山东段花岗岩锆石SHRIMP定年及其地球化学特征
  
关键词:eastern part of Bayan Har Mountains  granites  intracontinental orogenics  Zircon SHRIMP age
基金项目:国家地质大调查计划“青海省达日县、久治县幅1∶25万区域地质调查”项目(编号:20031300009)
作者单位E-mail
沙淑清 中国地质大学,北京100083 wzxmail@vip.sina.com 
王宗秀 中国地质科学院地质力学研究所,北京100081  
郭通珍 青海省地质调查院,青海西宁810012  
肖伟峰 中国地质科学院地质力学研究所,北京100081  
杨欣德 中国地质科学院地质力学研究所,北京100081  
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摘要:
Zircon SHRIMP Dating and Geochemical Characteristics of Granites in the Eastern Part of the Bayan Har Mountains
      In the eastern part of the Bayan Har Mountains, granites with the SHRIMP U-Pb age of 218197 Ma directly intruded folded Triassic strata and are unconformably covered by Jurassic Nianbao Formation. These granites, composed of granodiorite, adamellite and syenogranite, have porphyritoid or porphyritic texture and abundant aluminum and potassium. In addition, they are characterized by lots of biotites, some aluminum-rich minerals such as garnets and tourmalines, and some gray fine dioritic inclusions. With A/CNK 1.001.22, they should belong to CPG-type granite in Barbarin's classification. They were formed at the late stage of Bayan Har intracontinental orogenic activity.
SHA Shu-qing,WANG Zong-xiu,GUO Tong-zhen,XIAO Wei-feng,YANG Xin-de.2007.Zircon SHRIMP Dating and Geochemical Characteristics of Granites in the Eastern Part of the Bayan Har Mountains[J].Acta Geoscientica Sinica,28(3):261-269.
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