ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
巴颜喀拉地体POG型花岗岩同位素年代学研究
  
关键词:Ar- 40 Ar age  207 Pb/ 206 P age  isotope geochronolgy  Bayan Har terrain
基金项目:《东昆仑及其邻区岩石圈缩短机制研究》项目,地质行业基金
作者单位
陈文 中国地质科学院地质研究所 
Arnau,N 巴斯卡尔大学 
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摘要:
Isotope Geochronology Study for “POG Type” Granite in Bayan Har Terrain
      Bayan Har terrain lies in the northern part of the Tibet plateau, and between the Kunlun terrain and Qiantang terrain. there are many granite outcrops in the eastern part of Bayanhar terrain. The 39 Ar- 40 Ar age of biotite and the 207 Pb/ 206 Pb age of zircon indicate the granite body formed at 220~212 Ma. After that, the granite had undergone two times metamorphism and deformation at 148 Ma and 110Ma。
CHEN Wen,Arnau,N.1997.Isotope Geochronology Study for “POG Type” Granite in Bayan Har Terrain[J].Acta Geoscientica Sinica,18(3):261-266.
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