造山带橄榄岩中锆石的成因及其地质意义

郑建平; 赵伊; 熊庆

doi:10.3799/dqkx.2018.375

Volume 44 Issue 4

Apr. 2019

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Zheng Jianping, Zhao Yi, Xiong Qing, 2019. Genesis and Geological Significance of Zircons in Orogenic Peridotite. Earth Science, 44(4): 1067-1082. doi: 10.3799/dqkx.2018.375

Citation:

Zheng Jianping, Zhao Yi, Xiong Qing, 2019. Genesis and Geological Significance of Zircons in Orogenic Peridotite. Earth Science, 44(4): 1067-1082. doi: 10.3799/dqkx.2018.375

Zheng Jianping, Zhao Yi, Xiong Qing, 2019. Genesis and Geological Significance of Zircons in Orogenic Peridotite. Earth Science, 44(4): 1067-1082. doi: 10.3799/dqkx.2018.375

Citation:

Zheng Jianping, Zhao Yi, Xiong Qing, 2019. Genesis and Geological Significance of Zircons in Orogenic Peridotite. Earth Science, 44(4): 1067-1082. doi: 10.3799/dqkx.2018.375

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Genesis and Geological Significance of Zircons in Orogenic Peridotite

doi: 10.3799/dqkx.2018.375

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2018-09-19
Publish Date: 2019-04-15

Abstract

Abstract

Orogenic peridotites record the complex geological processes of continental subduction, collision and exhumation, and they can be divided into two types: crustal origin and mantle origin. Zircons are rarely found in orogenic peridotites. The in-situ zircons and zircon inclusions with mantle-rock mineral assemblages indicate that the zircons can grow within the peridotites. During the complex processes of plate aggregation (such as UHP metamorphism), the orogenic peridotites experienced the melt/fluid interaction in different periods, which have an important impact on the mineral and elemental compositions of peridotites. Zircon is one of the typical metasomatic minerals of orogenic peridotites. The zircon formation is controlled by the composition of the melt/fluid, source properties, and the formation of a physical and chemical environment. The mantle-derived zircons from orogenic peridotites have three origins:(1) Zircon has strong crystallization ability, and Zr prefers to combine with Si from silicate minerals in mantle rocks to form zircons. (2) Metamorphic destruction of Zr-bearing mineral phases and precipitation from intergranular melts generated can nucleate zircons under sub-solidus conditions. (3) The melt/fluid from the recycled crust can metasomatize the mantle wedge and form zircons. Thus, zircons can be used to unravel the history of specific lithospheric domains and thus contribute to our understanding of the evolution of continental cratons and their margins.
- orogenic peridotite,
- origin of zircon,
- crystallization capacity,
- Zr saturation,
- mantle metasomatism,
- petrology

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References(112)

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Genesis and Geological Significance of Zircons in Orogenic Peridotite

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