晶粥储存、侵入体累积组装与花岗岩成因

马昌前; 邹博文; 高珂; 文霞

doi:10.3799/dqkx.2020.316

Volume 45 Issue 12

Dec. 2020

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Ma Changqian, Zou Bowen, Gao Ke, Wen Xia, 2020. Crystal Mush Storage, Incremental Pluton Assemblyand Granitic Petrogenesis. Earth Science, 45(12): 4332-4351. doi: 10.3799/dqkx.2020.316

Citation:

Ma Changqian, Zou Bowen, Gao Ke, Wen Xia, 2020. Crystal Mush Storage, Incremental Pluton Assemblyand Granitic Petrogenesis. Earth Science, 45(12): 4332-4351. doi: 10.3799/dqkx.2020.316

Ma Changqian, Zou Bowen, Gao Ke, Wen Xia, 2020. Crystal Mush Storage, Incremental Pluton Assemblyand Granitic Petrogenesis. Earth Science, 45(12): 4332-4351. doi: 10.3799/dqkx.2020.316

Citation:

Ma Changqian, Zou Bowen, Gao Ke, Wen Xia, 2020. Crystal Mush Storage, Incremental Pluton Assemblyand Granitic Petrogenesis. Earth Science, 45(12): 4332-4351. doi: 10.3799/dqkx.2020.316

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Crystal Mush Storage, Incremental Pluton Assemblyand Granitic Petrogenesis

doi: 10.3799/dqkx.2020.316

Ma Changqian^{1, 2
,
,},
Zou Bowen¹,
Gao Ke¹,
Wen Xia³

1.
School of Earth Science, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
3.
School of Resource Environment and Safety Engineering, University of South China, Hengyang 421001, China

Received Date: 2020-08-24
Publish Date: 2020-12-15

Abstract

Abstract

Storage,migration and differentiation of granitic magma in the crust are the basic processes leading to the growth and evolution of continental crust. Studies of magma storage and assembly in the crust over the past decade have challenged traditionally-held views of magma chambers as large,molten melt bodies. Geophysical exploration,petrological and mineralogical studies,and thermal history simulations in active volcanic areas have consistently demonstrated that the material in magma reservoirs is mainly crystal mush residing under sub-solidus temperature conditions for a long time and remaining in relatively cold storage. The large plutons outcropping on the surface today represent fossil magma reservoirs. Most of them were formed by multiple additions and incremental assembly of magma over a span of millions of years or even longer. The incremental assembly of plutons can be proved by observation of contact relationships between intrusive units,heterogeneity of rock and mineral compositions,and large timescales of pluton emplacement. The intrusion of large plutons in a shallow crust and large-volume volcanic eruptions require the existence of transcrustal magma plumbing systems in which magma is connected by a series of dykes to magma reservoirs at different depths,and huge stocks and batholiths are assembled by stacking of numerous sills.The existence of highly-fractionated granites and high-silica rhyolites,and especially the phenomena of super-eruptions require the reactivation and differentiation of crystal mush in magma reservoirs. The disaggregation of crystal mush is often due to a fresh magma intrusion from below injecting additional heat and fluid. The crystal cargo can provide clues to the pluton assembly,crystal mush rejuvenation and magma differentiation. In particular,antecrysts can provide new insights into the evolution of magma plumbing systems. In future,the study of granitic petrogenesis will focus on crystal mush rejuvenation and magma differentiation,the mechanisms of magma rise and assembly,the genetic relationships between volcanic rocks and intrusive rocks,and interdisciplinary research on magma plumbing systems,in order to construct a new paradigm for the study of granitic magma processes,and in-depth understanding of the growth and evolution mechanisms of continental crust.
- crystal mush,
- magma reservoirs,
- magmatic plumbing system,
- cold storage,
- incremental assembly,
- granitoids

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References(161)

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Crystal Mush Storage, Incremental Pluton Assemblyand Granitic Petrogenesis

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