gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2017-8-3-0275gtcrust-416Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSTRIASSIC TERMINAL MAGMATISM IN THE SOUTHERN CENTRAL ASIAN OROGENIC BELT: IMPLICATIONS FOR OCEAN CLOSURE IN ACCRETIONARY OROGENSTRIASSIC TERMINAL MAGMATISM IN THE SOUTHERN CENTRAL ASIAN OROGENIC BELT: IMPLICATIONS FOR OCEAN CLOSURE IN ACCRETIONARY OROGENSLiShanLiShan

Beijing 100037

Beijing 100037

WangTaoWangTao

Beijing 100037

Beijing 100037

XiaoWen-JiaoXiaoWen-Jiao

Xinjiang Research Center for Mineral Resources, Urumqi 830011;

State Key Laboratory of Lithospheric Evolution, Beijing 100029

Xinjiang Research Center for Mineral Resources, Urumqi 830011;

State Key Laboratory of Lithospheric Evolution, Beijing 100029, China

ChungSun-LinChungSun-Lin

Taipei;

Department of Geosciences, Taipei

Taipei;

Department of Geosciences, Taipei

WildeSimon A.WildeSimon A.

Department of Applied Geology, 

Perth, Western Australia 6845

Department of Applied Geology, 

Perth, Western Australia 6845

Institute of Geology, Chinese Academy of Geological SciencesКитайInstitute of Geology, Chinese Academy of Geological SciencesChinaXinjiang Institute of Ecology and Geography, Chinese Academy of Sciences; Institute of Geology and Geophysics, Chinese Academy of SciencesКитайXinjiang Institute of Ecology and Geography, Chinese Academy of Sciences; Institute of Geology and Geophysics, Chinese Academy of SciencesChinaInstitute of Earth Sciences, Academia Sinica; National Taiwan UniversityТайваньInstitute of Earth Sciences, Academia Sinica; National Taiwan UniversityTaiwan, Province of ChinaCurtin UniversityАвстралияCurtin UniversityAustralia20171210201783507508Copyright © Li S., Wang T., Xiao W., Chung S., Wilde S., 20172017Li S., Wang T., Xiao W., Chung S., Wilde S.Li S., Wang T., Xiao W., Chung S., Wilde S.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/416

The key to defining the termination of accretion in an accretionary orogen is to recognize the initial magmatic processes that are generated at the time of ocean closure. We present new age, geochemical and isotopic data for magmatic rocks related to terminal collision along the Solonker-Xar Moron suture zone in the southern Central Asian Orogenic Belt (CAOB) that record such processes following closure of the PaleoAsian Ocean (Figure).

The key to defining the termination of accretion in an accretionary orogen is to recognize the initial magmatic processes that are generated at the time of ocean closure. We present new age, geochemical and isotopic data for magmatic rocks related to terminal collision along the Solonker-Xar Moron suture zone in the southern Central Asian Orogenic Belt (CAOB) that record such processes following closure of the PaleoAsian Ocean (Figure).

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