Some progress on understanding the Phanerozoic granitoids in China

Tao Wang; Ying Tong; Xiao-xia Wang; Jian-ren Mao; Hong-rui Zhang; He Huang; Shan Li; Lei Guo; Jian-jun Zhang

doi:10.31035/cg2018010

2018 Vol. 1, No. 1

Article Contents

Article navigation > China Geology > 2018 > 1(1): 84-108

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Tao Wang, Ying Tong, Xiao-xia Wang, Jian-ren Mao, Hong-rui Zhang, He Huang, Shan Li, Lei Guo, Jian-jun Zhang, 2018. Some progress on understanding the Phanerozoic granitoids in China, China Geology, 1, 84-108. doi: 10.31035/cg2018010

Citation:

Some progress on understanding the Phanerozoic granitoids in China

a.
Key Laboratory of Deep-Earth Dynamics, Ministry of Natural Resources, Beijing 100037, China
b.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
c.
Key Laboratory of Metallogeny and Mineral Assessment of Ministry of Natural Resources, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
d.
Nanjing center, China Geological Survey, Nanjing 210016, China

More Information

Corresponding author: Tao Wang E-mail: taowang@cags.ac.cn

Received Date: 07 December 2017

Revised Date: 10 January 2018

Accepted Date: 06 February 2018

Available Online: 10 March 2018

Publish Date: 25 March 2018

Abstract

Abstract

There are large volumes of the Phanerozoic granitoid rocks in China and neighboring areas. In recent years, numerous new and precise U-Pb zircon ages have been published for these granitoids, and define many important magmatic events, such as ca. 500 Ma granitoid events in the West Junggar, Altai orogens in the NW China, and Qinling orogen in the central China. These ages accurately constrain the time of important Early Paleozoic, Late Paleozoic, Early Mesozoic and Late Mesozoic magmatic events of the northern, central, western, southern and eastern orogenic Mountains in China. There occur various types of granitoids in China, such as calc-alkaline granite, alkali granite, highly-fractionated granite, leucogranite, adakite, and rapakivi granite. Rapakivi granites are not only typical Proterozoic as in the North China Craton, but were also emplaced during Paleozoic and Mesozoic in the Kunlun-Qinling orogen, a part of the China Central Orogenic Belt (CCOB). Nd-Hf isotopic tracing and mapping show that granitoids in the southern Central Asian Orogenic Belt (CAOB) in China (or the Northern China Orogenic Belt) are characterized predominantly by juvenile sources.The juvenile crust in this orogenic domain accounts for over 50% by area, distinguishing it from other orogenic belts in the world, and those in central (e.g., Qinling), southwestern and eastern China. Based on a large amount of new age data, a preliminary granitoid and granitoid-tectonic maps of China have been preliminarily compiled, and an evolutionary framework of Phanerozoic granitoids in China and neighboring areas has been established from the view of assembly and breakup of continental blocks. Research ideas on granitoid tectonics has also been proposed and discussed.
- Granitoids /
- zircon age /
- spatial-temporal distribution /
- radiogenic isotopes /
- orogen

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References

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