gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2017-8-3-0282gtcrust-423Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSNATURE OF THE LATE CARBONIFEROUS TO TRIASSIC MAGMATISM ALONG THE NORTHERN MARGIN OF THE NORTH CHINA BLOCK: LINK WITH THE EVOLUTION OF THE CENTRAL ASIAN OROGENNATURE OF THE LATE CARBONIFEROUS TO TRIASSIC MAGMATISM ALONG THE NORTHERN MARGIN OF THE NORTH CHINA BLOCK: LINK WITH THE EVOLUTION OF THE CENTRAL ASIAN OROGENPengPengPengPeng

State Key Laboratory of Lithospheric Evolution,

Beijing 100029

State Key Laboratory of Lithospheric Evolution, 

Chinese Academy of Sciences,

ZhaiMingguoZhaiMingguo

State Key Laboratory of Lithospheric Evolution,

Beijing 100029

State Key Laboratory of Lithospheric Evolution, 

Chinese Academy of Sciences,

SuXiangdongSuXiangdong

State Key Laboratory of Lithospheric Evolution,

Beijing 100029

State Key Laboratory of Lithospheric Evolution, 

Chinese Academy of Sciences,

ZhaoTaipingZhaoTaiping

Guangzhou 510640

Guangzhou 510640

ZhouYanyanZhouYanyan

State Key Laboratory of Lithospheric Evolution,

Beijing 100029

State Key Laboratory of Lithospheric Evolution, 

Chinese Academy of Sciences,

Institute of Geology and Geophysics, Chinese Academy of SciencesКитайInstitute of Geology and Geophysics, Chinese Academy of SciencesChinaGuangzhou Institute of Geochemistry, Chinese Academy of SciencesКитайGuangzhou Institute of Geochemistry, Chinese Academy of SciencesChina20171210201783531532Copyright © Peng P., Zhai M., Su X., Zhao T., Zhou Y., 20172017Peng P., Zhai M., Su X., Zhao T., Zhou Y.Peng P., Zhai M., Su X., Zhao T., Zhou Y.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/423

There are two episodes of magmatism along the northern margin of the North China block during the Late Carboniferous to Late Triassic, one at 310–250 Ma (Late Carboniferous to Permian) and the other at 235–210 Ma (Late Triassic). The former group comprises plutonic rocks (gabbro-diorite-monzodioritemonzogranite-granite), mafic to intermediate dykes (diorite to dolerite) and a few felsic volcanics (andesite to dacite).

There are two episodes of magmatism along the northern margin of the North China block during the Late Carboniferous to Late Triassic, one at 310–250 Ma (Late Carboniferous to Permian) and the other at 235–210 Ma (Late Triassic). The former group comprises plutonic rocks (gabbro-diorite-monzodioritemonzogranite-granite), mafic to intermediate dykes (diorite to dolerite) and a few felsic volcanics (andesite to dacite).

References

The authors declare that there are no conflicts of interest present.