大陆碰撞带深熔变质与花岗岩成因

郑永飞; 陈仁旭; 高彭

doi:10.3799/dqkx.2023.215

Volume 49 Issue 1

Jan. 2024

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Zheng Yongfei, Chen Renxu, Gao Peng, 2024. Anatectic Metamorphism and Granite Petrogenesis in Continental Collision Zones. Earth Science, 49(1): 1-28. doi: 10.3799/dqkx.2023.215

Citation:

Zheng Yongfei, Chen Renxu, Gao Peng, 2024. Anatectic Metamorphism and Granite Petrogenesis in Continental Collision Zones. Earth Science, 49(1): 1-28. doi: 10.3799/dqkx.2023.215

Zheng Yongfei, Chen Renxu, Gao Peng, 2024. Anatectic Metamorphism and Granite Petrogenesis in Continental Collision Zones. Earth Science, 49(1): 1-28. doi: 10.3799/dqkx.2023.215

Citation:

Zheng Yongfei, Chen Renxu, Gao Peng, 2024. Anatectic Metamorphism and Granite Petrogenesis in Continental Collision Zones. Earth Science, 49(1): 1-28. doi: 10.3799/dqkx.2023.215

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Anatectic Metamorphism and Granite Petrogenesis in Continental Collision Zones

doi: 10.3799/dqkx.2023.215

Zheng Yongfei^{1, 2, 3
,
,},
Chen Renxu^{1, 2, 3},
Gao Peng^{1, 2, 3}

1.
School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
2.
Key Laboratory of Crust-Mantle Materials and Environments, Chinese Academy of Sciences, Hefei 230026, China
3.
Center of Excellence for Comparative Planetology, Chinese Academy of Sciences, Hefei 230026, China

Received Date: 2023-11-14
Available Online: 2024-01-24
Publish Date: 2024-01-25

Abstract

Abstract

Anatectic metamorphism develops from high-grade metamorphism to crustal anataxis, marking population of extensional tectonism in continental collision zones. It is much more related to breakup than assembly of supercontinents in both space and time.Deciphering the anatectic metamorphism is critical to understand the tectonic evolution of continental collision zones in the late stage. It is substantial to resolve not only petrological problems such as crustal differentiation and granite petrogenesis but also tectonic problems such as supercontinent geodynamics in Wilson cycles. In general, continental collision zones may change their dynamic regime from compression to extension and their geothermal gradient from low to high during their evolution from the early to late stages. This results in different types of metamorphism and magmatism with given occurrences in both time and space. Alpine type metamorphism is caused by compressional heating at low geothermal gradients during subduction of one lithosphere beneath the others, and Barrovian type metamorphism occurs at moderate geothermal gradients due either to compressional heating during collisional thickening of the crust or to extensional decompression during nearly isothermal exhumation of the deeply subducted crust. In contrast, Buchan type metamorphism is caused by extensional heating at high geothermal gradients during continental rifting. Because of the anatectic metamorphism, granites are produced together with migmatites and granulites in the post-collisional stage. Therefore, granitic magmatism is the endmember product of anatectic metamorphism consequential to thinning of the thickened lithospheric mantle. Both processes are closely associated with the change of lithospheric thickness along continental collision zones. Although granites above oceanic subduction zone are mainly produced by fractional crystallization of mantle-derived mafic magmas, partial melting of crustal rocks is the dominant way to generate granitic magmas in continental collision zones. In particular, the source nature of crustal rocks is a key to the composition of granites. Ⅰ-type and S-type granites are primarily derived from partial melting of metaigneous and metasedimentary rocks, respectively. In comparison, A-type granites are derived from partial melting of either cumulates or restites. Dehydration and hydration melting are two fundamental mechanisms to produce granitic magmas. They can occur simultaneously at the same zones, leading to dehydration melting in the deeper crust and hydration melting in the shallower crust. Upwelling of the asthenospheric mantle consequential to thinning of the lithospheric mantle is a common geodynamic mechanism for continental active rifting, giving rise to the dehydration-hydration coupled melting to produce granite-migmatite-granulite associations in continental collision zones. As a consequence, supercontinent assembly is associated with compressional metamorphism during continental collision, whereas supercontinent breakup is associated with extensional metamorphism during active rifting. Continent rifting may not succeed but fail, resulting in anatectic metamorphism and granitic magmatism at convergent plate margins. Therefore, the failed continental rifting is a key process in linking the types of regional metamorphism to the tectonic evolution of continental collision zones from supercontinent assembly to breakup.
- continental collision,
- anatectic metamorphism,
- granitic magmatism,
- continental rifting,
- intracontinental orogeny,
- chemical geodynamics,
- convergent plate margin

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References(155)

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Anatectic Metamorphism and Granite Petrogenesis in Continental Collision Zones

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