Polymetamorphism of the ultrahigh-temperature granulites in the Rauer Group,East Antarctica:new evidence from zircon SHRIMP U-Pb agesOA
Polymetamorphism of the ultrahigh-temperature granulites in the Rauer Group,East Antarctica:new evidence from zircon SHRIMP U-Pb ages
TONG Laixi;LIU Zhao;LI Chao;LU Junsheng;YANG Wenqiang;WANG Yanbin
State Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi'an 710069,ChinaState Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi'an 710069,ChinaState Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi'an 710069,ChinaState Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi'an 710069,ChinaState Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi'an 710069,ChinaInstitute of Geology,Chinese Academy of Geological Sciences,Bejing 100037,China
ultrahigh-temperature granuliteszircon SHRIMP U-Pb agespolymetamorphismRauer GroupEast Antarctica
ultrahigh-temperature granuliteszircon SHRIMP U-Pb agespolymetamorphismRauer GroupEast Antarctica
《极地科学进展（英文版）》 2024 (2)
192-205,14
The field work was carried out with logistic support from the 27th and 33rd Chinese National Antarctic Research Expedition(CHINARE)during 2010/2011 and 2016/2017.The zircon isotopic analyses were finished by help of Dr.Jianhui Liu and Dr.Runlong Fan at the Beijing SHRIMP Centre,Chinese Academy of Geological Sciences.This study has been financially supported by the National Nature Science Foundation of China(Grant no.41972050).Constructive reviews and comments on the manuscript by two anonymous reviewers and Associate Editor Dr.Shi Xuefa are very much appreciated.
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