ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
中亚造山带南缘中—新元古代地壳的揭示——来自北山—阿拉善北部钻遇碱性花岗岩的年代学和Hf同位素示踪研究
  
关键词:microcontinent  Beishan  Alxa  alkaline granite  Late Carboniferous  zircon U-Pb  LA-ICP-MS  Lu-Hf
基金项目:中国地质调查局地质调查项目(编号: DD20190092; DD20190113)
作者单位E-mail
宋博 中国科学院大学地球与行星科学学院
中国地质调查局西安地质调查中心
中国地质调查局北方古生界油气地质重点实验室 
sbo@cgs.cn 
张慧元 中国地质调查局西安地质调查中心
中国地质调查局北方古生界油气地质重点实验室 
 
魏东涛 中国地质调查局西安地质调查中心
中国地质调查局北方古生界油气地质重点实验室 
 
李渭 中国地质调查局西安地质调查中心
中国地质调查局北方古生界油气地质重点实验室 
 
赵飞 中国地质调查局西安地质调查中心
中国地质调查局北方古生界油气地质重点实验室 
 
李文明 中国地质调查局西安地质调查中心
中国地质调查局北方古生界油气地质重点实验室 
 
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摘要:
Revelation of the Meso–Neoproterozoic Crust on the Southern Margin of the Central Asian Orogenic Belt: Chronology and Hf Isotope Tracer from Drilling-intersected Alkaline Granites, Northern Beishan–Alxa
      The Precambrian microcontinent is an important component of the northern Beishan–Alxa accretionary orogenic belt. Much controversy exists regarding the Precambrian basement of the Hanshan, Yagan and Zhusileng–Hangwula. Juyanhai is located between the northern part of the Beishan Orogenic Belt and the northern margin of the Alxa block. It is restricted by the Badain Jaran Desert and has very few rock outcrops. The authors drilled a set of Late Carboniferous alkaline granites. The zircon LA-ICP-MS U-Pb chronology and Hf isotope characteristics reveal that the granitic magma has zircon crystallization ages of (312 ± 1) Ma and (315 ± 2) Ma, and has positive εHf(t) values between + 0.8 and + 4.4, +2.2 on average, corresponding to the two-stage model age (TDM2) of 1048 ~ 1267 Ma, with average value being 1183 Ma. The ancient crust contributed the granitic magma. Based on comparing the Late Carboniferous granitoids with the Hanshan tectonic Belt, Queershan tectonic Belt, Yagan tectonic Belt, and Zhusleng–Hangwula tectonic Belt, the authors analyzed the Meso–Neoproterozoic crust in northern Beishan–Alxa. Additionally, based on the outcrops of 0.9 Ga granitic rocks and the regional interpretation of gravity and magnetic data, the authors infer that the Hanshan, Yagan and Zhusileng–Hangwula tectonic belts assembled together, and further conjunction can be carried out.
SONG Bo,ZHANG Hui-yuan,WEI Dong-tao,LI Wei,ZHAO Fei,LI Wen-ming.2021.Revelation of the Meso–Neoproterozoic Crust on the Southern Margin of the Central Asian Orogenic Belt: Chronology and Hf Isotope Tracer from Drilling-intersected Alkaline Granites, Northern Beishan–Alxa[J].Acta Geoscientica Sinica,42(1):9-20.
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