gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2017-8-3-0299gtcrust-440Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSOUTLINE OF GRANITOIDS OF THE CENTRAL ASIA OROGENIC BELT: FOCUSED ON THE SOUTHERN PARTOUTLINE OF GRANITOIDS OF THE CENTRAL ASIA OROGENIC BELT: FOCUSED ON THE SOUTHERN PARTWangT.WangT.

Beijing 100037

Beijing 100037

TongY.TongY.

Beijing 100037

Beijing 100037

ZhangL.ZhangL.

Beijing 100037

Beijing 100037

LiS.LiS.

Beijing 100037

Beijing 100037

HuangH.HuangH.

Beijing 100037

Beijing 100037

ZhangJ. J.ZhangJ. J.

Beijing 100037

Beijing 100037

GuoL.GuoL.

Beijing 100037

Beijing 100037

YangQ. D.YangQ. D.

Beijing 100037

Beijing 100037

HongD. W.HongD. W.

Beijing 100037

Beijing 100037

DonskayaT.DonskayaT.

Irkutsk 664033

Irkutsk 664033

GladkochubD.GladkochubD.

Irkutsk 664033

Irkutsk 664033

NarantsetsegTs.NarantsetsegTs.

Ulaanbaatar 15160

Ulaanbaatar 15160

Institute of Geology, Chinese Academy of Geological Sciences; Beijing SHRIMP Center, Chinese Academy of Geological, SciencesКитайInstitute of Geology, Chinese Academy of Geological Sciences; Beijing SHRIMP Center, Chinese Academy of Geological, SciencesChinaInstitute of Geology, Chinese Academy of Geological SciencesКитайInstitute of Geology, Chinese Academy of Geological SciencesChinaInstitute of the Earth’s Crust, Siberian Branch of RASРоссияInstitute of the Earth’s Crust, Siberian Branch of RASRussian FederationInstitute of Paleontology and Geology, Mongolian Academy of SciencesМонголияInstitute of Paleontology and Geology, Mongolian Academy of SciencesMongolia20171410201783589591Copyright © Wang T., Tong Y., Zhang L., Li S., Huang H., Zhang J.J., Guo L., Yang Q.D., Hong D.W., Donskaya T., Gladkochub D., Narantsetseg T., 20172017Wang T., Tong Y., Zhang L., Li S., Huang H., Zhang J.J., Guo L., Yang Q.D., Hong D.W., Donskaya T., Gladkochub D., Narantsetseg T.Wang T., Tong Y., Zhang L., Li S., Huang H., Zhang J.J., Guo L., Yang Q.D., Hong D.W., Donskaya T., Gladkochub D., Narantsetseg T.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/440

The Central Asian Orogenic Belt (CAOB), bounded by the Siberian craton to the north and the TarimNorth China cratons to the south, is a complex collage of microcontinental blocks, island arcs, oceanic crustal remnants and continental marginal facies rocks. It is one of the largest and most complex accretionary orogenic belts and the most important site of Phanerozoic continental growth on the Earth [Jahn et al., 2000, 2004; Kovalenko et al., 2004] The widespread occurrence of large volumes of granitoids, mostly with juvenile sources, is a typical characteristic of the CAOB. These granitoids have been intensely studied (e.g. [Jahn et al., 2000, 2004; Kovalenko et al., 2004; Sorokin et al., 2004; Vladimirov et al., 2001; Han et al., 2010; Wang et al., 2006, 2015; Wu et al., 2011; Li et al., 2013; Yarmolyuk et al., 2002]). However, these studies mainly focused on some certain countries or regions.

the Siberian craton to the north and the TarimNorth China cratons to the south, is a complex collage of microcontinental blocks, island arcs, oceanic crustal remnants and continental marginal facies rocks. It is one of the largest and most complex accretionary orogenic belts and the most important site of Phanerozoic continental growth on the Earth [Jahn et al., 2000, 2004; Kovalenko et al., 2004] The widespread occurrence of large volumes of granitoids, mostly with juvenile sources, is a typical characteristic of the CAOB. These granitoids have been intensely studied (e.g. [Jahn et al., 2000, 2004; Kovalenko et al., 2004; Sorokin et al., 2004; Vladimirov et al., 2001; Han et al., 2010; Wang et al., 2006, 2015; Wu et al., 2011; Li et al., 2013; Yarmolyuk et al., 2002]). However, these studies mainly focused on some certain countries or regions.

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