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Geochronology, petrogenesis, and tectonic implications of Permian felsic rocks of the Central Great Xing’an Range, NE China

  • Yong-Fei Ma
  • Yong-Jiang LiuEmail author
  • Yan Wang
  • Cheng Qian
  • Qiu-Liang Si
  • Zhen Tang
  • Tao Qin
Original Paper
  • 147 Downloads

Abstract

The Hegenshan–Heihe Suture (HHS) is an important suture zone between the Xing’an and Songliao–Xilinhot blocks in the eastern Central Asian Orogenic Belt (CAOB). Many studies have examined the northern and southern parts of this suture zone, but the middle segment remains under-researched and controversial. This paper presents new research into Permian felsic rocks along the middle segment of the HHS, including alkaline granites, rhyolites, and granodiorites. Zircon U–Pb dating of these rocks yielded precise Permian ages of 300.4 ± 2.5, 292.8 ± 2.7, and 293.1 ± 2.2 Ma. The alkaline granites and the rhyolites are A-type rocks that were derived from lower crustal protoliths, with the melting of these protoliths caused by asthenospheric upwelling associated with lithospheric delamination. In comparison, the granodiorites are I-type granites were generated from a mantle-derived magmatic source. The petrogenesis of these granites also involved the assimilation of sedimentary rocks and fractional crystallization. This Permian magmatism occurred during post-collisional extension following the amalgamation of the Xing’an and Songliao–Xilinhot blocks.

Keywords

Hegenshan–Heihe Suture Permian Felsic rocks Geochronology Petrogenesis Tectonic setting 

Notes

Acknowledgements

This work was financially supported by the National Key R&D Program of China (Grant 2017YFC0601300-01) and 973 Program (Grant 2013CB429802), and the Scientific and Technological Innovation Project Financially Supported by Qingdao National Laboratory for Marine Science and Technology (Grants 2015ASKJ01), the China Geological Survey (Grants 12120113053800 and DD20160201-03), and the National Natural Science Foundation of China (Grants 41602235). We are very grateful to Dr. Chen Huijun and the other anonymous reviewers for their thoughtful and constructive reviews of this manuscript. We also thank the staff of the National Research Center for Geoanalys, Chinese Academy of Geological Sciences, Beijing, China, for helping with the zircon LA–ICP–MS U–Pb dating, Northeast China Supervision and Inspection Center of Mineral Resources, Ministry of Land and Resources, Shenyang, China, for helping with the whole-rock major and trace-element analyses.

Supplementary material

531_2018_1661_MOESM1_ESM.doc (396 kb)
Supplementary material 1 (DOC 395 KB)

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Copyright information

© Springer-Verlag GmbH Germany, part of Springer Nature 2018

Authors and Affiliations

  1. 1.Shenyang Center, China Geological Survey (CGS)ShenyangChina
  2. 2.College of Earth SciencesJilin UniversityChangchunChina
  3. 3.Key Lab of Submarine Geosciences and Prospecting Techniques, Ministry of Education, and College of Marine GeosciencesOcean University of ChinaQingdaoChina
  4. 4.Laboratory for Marine Mineral ResourcesQingdao National Laboratory for Marine Science and TechnologyQingdaoChina

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