汇聚板块边缘从大洋俯冲经大陆碰撞到碰撞后再造过程中的碳循环

苏懿; 李姝宁; 陈仁旭; 郑永飞

doi:10.3799/dqkx.2025.060

Volume 50 Issue 8

Aug. 2025

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Su Yi, Li Shuning, Chen Renxu, Zheng Yongfei, 2025. Deep Carbon Cycle during Tectonic Evolution from Oceanic Subduction through Continental Collision to Post-Collisional Reworking at Convergent Plate Margins. Earth Science, 50(8): 3085-3116. doi: 10.3799/dqkx.2025.060

Citation:

Su Yi, Li Shuning, Chen Renxu, Zheng Yongfei, 2025. Deep Carbon Cycle during Tectonic Evolution from Oceanic Subduction through Continental Collision to Post-Collisional Reworking at Convergent Plate Margins. Earth Science, 50(8): 3085-3116. doi: 10.3799/dqkx.2025.060

Citation:

Su Yi, Li Shuning, Chen Renxu, Zheng Yongfei, 2025. Deep Carbon Cycle during Tectonic Evolution from Oceanic Subduction through Continental Collision to Post-Collisional Reworking at Convergent Plate Margins. Earth Science, 50(8): 3085-3116. doi: 10.3799/dqkx.2025.060

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Deep Carbon Cycle during Tectonic Evolution from Oceanic Subduction through Continental Collision to Post-Collisional Reworking at Convergent Plate Margins

doi: 10.3799/dqkx.2025.060

Su Yi^{1, 2
,
,},
Li Shuning¹,
Chen Renxu^{2
,
,
,},
Zheng Yongfei^{1, 2}

1.
MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China
2.
State Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China

Received Date: 2025-02-19
Publish Date: 2025-08-25

Abstract

Abstract

The deep carbon cycle significantly influences atmospheric CO₂ concentrations, playing a critical role in global climate change and Earth's habitability. At convergent plate margins, surface carbon undergoes deep cycling through plate subduction via a series of processes such as metamorphic dehydration and/or partial melting, crust-mantle interactions, and magmatism. This paper presents a systematical review on the carbon reservoirs of the mantle and crust, the decarbonation mechanisms in subducting slabs, carbon sequestration during crust-mantle interactions, and the role of magmatic activity at convergent plate margins in deep carbon cycling and carbon release. It also outlines the footprints of deep carbon cycling in oceanic subduction zones and continental collision zones, along with the factors affecting carbon release, sequestration, or migration in various processes.
- convergent plate margin,
- deep carbon cycle,
- crust-mantle interaction,
- decarbonization mechanism,
- continental reworking,
- tectonics

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References(246)

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Deep Carbon Cycle during Tectonic Evolution from Oceanic Subduction through Continental Collision to Post-Collisional Reworking at Convergent Plate Margins

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