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Volume 30 Issue 4
Aug 2019
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Journal of Earth Science  > 2019  >  30(4): 689-706.
Jinhua Qin, Cui Liu, Yuchuan Chen, Jinfu Deng. Timing of Lithospheric Extension in Northeastern China: Ev-idence from the Late Mesozoic Nianzishan A-Type Granitoid Complex. Journal of Earth Science, 2019, 30(4): 689-706. doi: 10.1007/s12583-018-0996-9
Citation: Jinhua Qin, Cui Liu, Yuchuan Chen, Jinfu Deng. Timing of Lithospheric Extension in Northeastern China: Ev-idence from the Late Mesozoic Nianzishan A-Type Granitoid Complex. Journal of Earth Science, 2019, 30(4): 689-706. doi: 10.1007/s12583-018-0996-9
shu

Timing of Lithospheric Extension in Northeastern China: Ev-idence from the Late Mesozoic Nianzishan A-Type Granitoid Complex

doi: 10.1007/s12583-018-0996-9
  • 1.

    MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, CAGS, Beijing 100037, China

  • 2.

    School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

More Information
  • Corresponding author: Cui Liu
  • Received Date: 07 Sep 2018
  • Accepted Date: 03 Dec 2018
  • Publish Date: 01 Aug 2019
    Abstract
  • New zircon U-Pb dates obtained by laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS), whole-rock geochemical data and Sm-Nd and Rb-Sr isotopic data are presented for miarolitic alkaline granites, porphyritic syenite and rhyolites of the Nianzishan A-type granitoid complex (NAGC) in the Great Xing'an Range-Songliao Basin in Northeast (NE) China. New crystallization ages of 112.95±0.93 and 114.1±1.71 Ma for granite and 118.6±0.51 Ma for porphyritic syenite were determined by high-precision LA-ICP-MS. The εNd(t) of the rocks range from +1.85 to +2.06, with Nd model ages (TDM1) from 671 to 821 Ma, indicating that the NAGC originated from juvenile source rocks and exhibits geochemical characteristics of A1-and AA-type granite which formed in an extensional setting. We attribute the magmatism to regional extension and lithospheric thinning caused by the subduction of the western Pacific Plate about 120 to 100 Ma.

     

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