ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
甘肃北山野马泉岩体同位素地球化学特征
  
关键词:Sm-Nd-Pb isotope compositions  petrogenesis  Yemaquan granitic complex  Beishan in Gansu Province
基金项目:本文为国防科工委放射性废物治理专项研究成果。
作者单位E-mail
范洪海 核工业北京地质研究院北京100029 fhh270@263.net 
阂茂中 南京大学地球科学系江苏南京210093  
陈佳 南京大学地球科学系江苏南京210093  
季瑞利 核工业北京地质研究院北京100029  
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摘要:
Isotopic Geochenical Characteristics of Yemaquan Granitic Intrusions in Beishan Area, Gansu Province
      Sm-Nd-Pb isotope compositions reveal that I-type granite characteristics of the Ⅰ、Ⅱ Yemaquan intrusions are as follows:(87Sr/86Sr)i=0.708~0.710, εNd=-2.2291~-5.8664,and the plot of 207Pb/204Pb versus 206Pb/204Pb is near and below the evolutionary curve of the orogenic belt. The granitoids are characterized by mixed (crust+mantle) origin of rock-forming materials.The Ⅲ granitoid is S-type granite, whose (87Sr/86Sr), are 0.7149-0.7358 andεNd are-7.3750~-8.9556. The geodynamic environment of the granitoids was the Beishan orogenic belt related to intercontinental collision, especially at the time when collision was drawing to its end.
FAN Honghai,MIN Maozhon,CHEN Jia,JI Ruili.2005.Isotopic Geochenical Characteristics of Yemaquan Granitic Intrusions in Beishan Area, Gansu Province[J].Acta Geoscientica Sinica,26(z1):78-83.
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