典型文献
Crustal growth of the North China Craton at ca.2.5 Ga
文献摘要：
The prominent age peak at 2.7 billion years ago(Ga)revealed in global zircon data may represent a widespread formation event of substantial amounts of juvenile continental crust,that is,the new crust was extracted from mantle melting without reworking large amounts of ancient crustal material[1,2].In contrast to the 2.7 Ga peak exhibited by the global zircon age dataset,younger such events are only represented in certain areas of the world.For instance,another prominent,but younger event at 2.5 Ga is well-represented in the North China Craton(NCC),the Dharwar Craton of India,and the Gawler Craton of Australia[1].The widespread 2.7 Ga zircon age peak in the global age spectrum is commonly interpreted as Earth's peak of continental crustal production.How-ever,the age of major crustal generation of the North China Craton(NCC)still remains controversial.
文献关键词：
中图分类号：
作者姓名：
Peng Liou;Jinghui Guo;Peng Peng;Ross N.Mitchell;Mengxia Mao;Neng Jiang;Mingguo Zhai
作者机构：
State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;College of Earth and Planetary Sciences,University of Chinese Academy of Sciences,Beijing 100049,China
文献出处：
引用格式：
[1]Peng Liou;Jinghui Guo;Peng Peng;Ross N.Mitchell;Mengxia Mao;Neng Jiang;Mingguo Zhai-.Crustal growth of the North China Craton at ca.2.5 Ga)[J].科学通报（英文版）,2022(15):1553-1555
A类：
Dharwar,Gawler
B类：
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AB值：
0.508347
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