西秦岭印支早期铁堂峡石英正长斑岩的地球化学特征及其地质意义

赵东辉; 平先权; 郑建平; 艾磊; 邓昊

doi:10.3799/dqkx.2019.225

Volume 44 Issue 12

Dec. 2019

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Article Navigation > Earth Science > 2019 > 44(12): 4203-4221

Zhao Donghui, Ping Xianquan, Zheng Jianping, Ai Lei, Deng Hao, 2019. Geochemistry and Its Geological Significance of the Quartz Syenites in the Early Indosinian from the Tietang Gorge, West Qinling. Earth Science, 44(12): 4203-4221. doi: 10.3799/dqkx.2019.225

Citation:

Zhao Donghui, Ping Xianquan, Zheng Jianping, Ai Lei, Deng Hao, 2019. Geochemistry and Its Geological Significance of the Quartz Syenites in the Early Indosinian from the Tietang Gorge, West Qinling. Earth Science, 44(12): 4203-4221. doi: 10.3799/dqkx.2019.225

Citation:

Zhao Donghui, Ping Xianquan, Zheng Jianping, Ai Lei, Deng Hao, 2019. Geochemistry and Its Geological Significance of the Quartz Syenites in the Early Indosinian from the Tietang Gorge, West Qinling. Earth Science, 44(12): 4203-4221. doi: 10.3799/dqkx.2019.225

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Geochemistry and Its Geological Significance of the Quartz Syenites in the Early Indosinian from the Tietang Gorge, West Qinling

doi: 10.3799/dqkx.2019.225

1.
School of Lisiguang, China University of Geosciences, Wuhan 430074, China
2.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2019-08-03
Publish Date: 2019-12-15

Abstract

Abstract

A large number of small-scale dykes are located in the eastern part of the West Qinling, but they are lack of detailed study. Based on the detailed field work and petrological research, zircon U-Pb geochronology, geochemistry and zircon Lu-Hf isotope studies were carried out for the quartz syenites in the Tietang Gorge from Tianshui, West Qinling. The zircon U-Pb dating shows the crystallization ages of the quartz syenites are~250 Ma, indicating that they were formed in the Early Indosinian. Geochemistry research shows that the Tietang Gorge quartz syenites belong to the series of high-alkaline calc-alkaline rocks with weakly peraluminous. They have some adakitic characteristics with high Mg^#, enrichment in Ba, Sr, K and strong depletion in Nb and Ta, and no significant Eu anomalies. The zircon ε_Hf(t) for the quartz syenites ranges from -1.44 to +3.17, and the one-stage Hf model ages (t_DM1) vary from 765 to 945 Ma. The Tietang Gorge quartz syenites formed in the continental marginal arc environment of the northward subduction of the Animaqing Ocean. They derived from the partial melting of the subduction oceanic crust with its overlying sediment interacted with the mantle wedge, and a slight fractional crystallization occurred in their shallow magma chamber.
- quartz syenite,
- zircon U-Pb dating,
- zircon Lu-Hf isotope,
- Early Indosinian,
- West Qinling,
- petrology

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References(107)

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