俯冲带岩浆作用与大陆地壳生长

马超; 汤艳杰; 英基丰

doi:10.3799/dqkx.2019.026

Volume 44 Issue 4

Apr. 2019

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Ma Chao, Tang Yanjie, Ying Jifeng, 2019. Magmatism in Subduction Zones and Growth of Continental Crust. Earth Science, 44(4): 1128-1142. doi: 10.3799/dqkx.2019.026

Citation:

Ma Chao, Tang Yanjie, Ying Jifeng, 2019. Magmatism in Subduction Zones and Growth of Continental Crust. Earth Science, 44(4): 1128-1142. doi: 10.3799/dqkx.2019.026

Ma Chao, Tang Yanjie, Ying Jifeng, 2019. Magmatism in Subduction Zones and Growth of Continental Crust. Earth Science, 44(4): 1128-1142. doi: 10.3799/dqkx.2019.026

Citation:

Ma Chao, Tang Yanjie, Ying Jifeng, 2019. Magmatism in Subduction Zones and Growth of Continental Crust. Earth Science, 44(4): 1128-1142. doi: 10.3799/dqkx.2019.026

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Magmatism in Subduction Zones and Growth of Continental Crust

doi: 10.3799/dqkx.2019.026

Ma Chao^{1,2
,},
Tang Yanjie^{1
,
,},
Ying Jifeng¹

1.
State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
2.
University of Chinese Academy of Sciences, Beijing 100049, China

Received Date: 2019-02-21
Publish Date: 2019-04-15

Abstract

Abstract

The origin, growth and reworking of continental crust have always been a hot topics in the international geosciences, and there are still some disputes, particularly about the mode and rate of continental crust growth.In order to discuss continental crustal growth style, it briefly reviews the research achievements of subduction-related magmatism and continental crustal growth.Subduction zones can be divided into oceanic-oceanic subduction zones, oceanic-continental subduction zones and continental-continental subduction zones, characterized by arc magmatic rocks.Subduction-related magmatism has been widely accepted as the main continental crustal growth style.At present, there are two hypotheses of the growth of continental crust:basalt model and andesite model.The basalt model mainly highlights the evolution of the new crust to the continental crust through the processes of delamination and relamination, while the andesite model emphasizes that the continental crust is directly formed in the magmatic arc environments of the subduction zones where andesitic magmas occur.Plate convergent boundaries such as subduction and collision zones are considered to be the main locations for the growth and reworking of the Phanerozoic continental crust, and subduction-related magmatism is of great significance to continental crustal growth.
- subduction zone,
- magmatic arc,
- magmatism,
- continental crust,
- crustal growth,
- tectonics,
- petrology

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References(125)

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Magmatism in Subduction Zones and Growth of Continental Crust

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