ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
祁连山金佛寺岩体的岩石学和同位素年代学研究
  
关键词:petrology isotope chronology  Jinfosi pluton  Qilian Mts.
基金项目:“格尔木-额济纳旗地学断面多学科综合调查研究”项目
作者单位
张德全 中国地质科学院地质研究所 
孙桂英 中国地质科学院地质研究所 
徐洪林 中国地质科学院地质研究所 
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摘要:
Petrology and Isotope Chronology of the Jinfosi Pluton,Qilian Mts. ,Gansu
      The Jinfosi pluton is located to the Southcast of Jiuquan(39°12′ 39°24′N, 98°30′ 99°12′E).Three intrusive stages have been recognized :the early stage (Jinfosi granodiorite-quartz mon-zonite(GQM );the middle stage of Dacaotan monzonitic granite(MG and the late stage of Gan-baou muscovite-biotite granite( MBG).The whole- rock Rb-Sr isochron age GQM is 419.87±0.4Ma and that of MG is 403.77±0.08Ma. The emplacement age is late silurian rather thanlate Devonian. The Jinfosi pluton’s ΣREE is (96.51-120.16) × 10 ̄6,δEu 0.67 0.77,εSr(t)+45. 8 ,and εNdt) 16.3. Its magma was derived by partial melting of the middle lower crust at adepth ranging from 30km to 36km. Since its formation ,the pluton has experienced three upliftevents(D,T,and N-Q)and two subsidence events(C and Cr.).
ZHANG De-quan,SUN Gui-ying,XU Hong-lin.1995.Petrology and Isotope Chronology of the Jinfosi Pluton,Qilian Mts. ,Gansu[J].Acta Geoscientica Sinica,16(4):375-385.
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