ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
东昆仑—西秦岭造山带对接处三叠纪花岗质岩石时空演化、物源特征对比及其大地构造意义
  
关键词:granitic rocks  zircon geochronology  Nd-Hf isotopic mapping  magmatism evolution  the eastern part of East Kunlun and the western part of West Qinling
基金项目:中国地质调查局项目(编号: 12120113094000; 1212010811033; 1212011120115; 20160123); 国家自然科学基金(编号: 41172062; 41572052)
作者单位E-mail
任海东 青海大学, 青藏高原北缘新生代资源环境重点实验室
中国地质科学院地质研究所
青海大学, 省部共建三江源生态与高原农牧业国家重点实验室 
mingqiangren@163.com 
王涛 中国地质科学院地质研究所 taowang@cags.ac.cn 
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摘要:
Temporal-spatial Variations, Sources and Tectonic Significances of the Triassic Granitic Rocks in the Junction Part of the East Kunlun and West Qinling Orogen, Central China
      The composition and evolution of orogen is the main subject of tectonic study, and the connection relationship between orogens is an important node in orogenic study. In the junction part of two orogenic belts, the contrast of tectonic-magmatic evolution between two orogens, especially contrast of deep crustal composition structure and basement affinity, can provide an important basis to completely under-stand the basement nature and tectonic affinity of the orogen. Based on its advantages in geochronology, regional widely distributed and easily tracing, Nd-Hf isotopic mapping for granitic rocks has gradually be-come an effective approach to delineate tec-tono-thermal evolution of the orogen, elucidate oro-genic composition and contrast basement nature be-tween two orogens.
REN Hai-dong,WANG Tao.2017.Temporal-spatial Variations, Sources and Tectonic Significances of the Triassic Granitic Rocks in the Junction Part of the East Kunlun and West Qinling Orogen, Central China[J].Acta Geoscientica Sinica,38(s1):59-63.
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