gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2017-8-3-0284gtcrust-425Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSAN EARLY PERMIAN GARNET-BEATING PERALUMINOUS GRANITIC PLUTON IN THE SOUTH TIANSHAN OROGENIC BELT, NW CHINA: PETROLOGICAL, MINERALOGICAL AND GEOCHEMICAL CONSTRAINTSAN EARLY PERMIAN GARNET-BEATING PERALUMINOUS GRANITIC PLUTON IN THE SOUTH TIANSHAN OROGENIC BELT, NW CHINA: PETROLOGICAL, MINERALOGICAL AND GEOCHEMICAL CONSTRAINTSQinQieQinQie

Beijing 100037

Beijing 100037

HuangHeHuangHe

Beijing 100037

Beijing 100037

WangTaoWangTao

Beijing 100037

Beijing 100037

ZhangZhaochongZhangZhaochong

State Key Laboratory of Geological Processes and Mineral Resources, 

Beijing 100083

State Key Laboratory of Geological Processes and Mineral Resources, 

Beijing 100083

Institute of Geology, Chinese Academy of Geological SciencesКитайInstitute of Geology, Chinese Academy of Geological SciencesChinaChina University of GeosciencesКитайChina University of GeosciencesChina20171310201783537538Copyright © Qin Q., Huang H., Wang T., Zhang Z., 20172017Qin Q., Huang H., Wang T., Zhang Z.Qin Q., Huang H., Wang T., Zhang Z.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/425

The Ku’erchu granitic pluton (283±4 Ma) was exposed in the eastern part of the South Tianshan Orogenic Belt. The granites from the intrusion are mainly composed of orthoclase (~45 vol. %), plagioclase (~15 vol. %), quartz (~20 vol. %), muscovite (~10 vol. %) and biotite (~5 vol. %), with accessory minerals including garnet, zircon and Fe-Ti oxide.

The Ku’erchu granitic pluton (283±4 Ma) was exposed in the eastern part of the South Tianshan Orogenic Belt. The granites from the intrusion are mainly composed of orthoclase (~45 vol. %), plagioclase (~15 vol. %), quartz (~20 vol. %), muscovite (~10 vol. %) and biotite (~5 vol. %), with accessory minerals including garnet, zircon and Fe-Ti oxide.

References

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