浙西开化地区新元古代(~800 Ma)洋陆俯冲:来自活动陆缘弧火山岩序列组合的制约

唐增才; 汪发祥; 周汉文; 吴小勇; 陈忠大; 胡开明; 赵旭东; 董学发; 余盛强; 胡文杰

doi:10.3799/dqkx.2018.244

Volume 45 Issue 1

Jan. 2020

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Article Navigation > Earth Science > 2020 > 45(1): 180-193

Tang Zengcai, Wang Faxiang, Zhou Hanwen, Wu Xiaoyong, Chen Zhongda, Hu Kaiming, Zhao Xudong, Dong Xuefa, Yu Shengqiang, Hu Wenjie, 2020. Neoproterozoic (~800 Ma) Subduction of Ocean-Continent Transition: Constraint from Arc Magmatic Sequence in Kaihua, Western Zhejiang. Earth Science, 45(1): 180-193. doi: 10.3799/dqkx.2018.244

Citation:

Tang Zengcai, Wang Faxiang, Zhou Hanwen, Wu Xiaoyong, Chen Zhongda, Hu Kaiming, Zhao Xudong, Dong Xuefa, Yu Shengqiang, Hu Wenjie, 2020. Neoproterozoic (~800 Ma) Subduction of Ocean-Continent Transition: Constraint from Arc Magmatic Sequence in Kaihua, Western Zhejiang. Earth Science, 45(1): 180-193. doi: 10.3799/dqkx.2018.244

Citation:

Tang Zengcai, Wang Faxiang, Zhou Hanwen, Wu Xiaoyong, Chen Zhongda, Hu Kaiming, Zhao Xudong, Dong Xuefa, Yu Shengqiang, Hu Wenjie, 2020. Neoproterozoic (~800 Ma) Subduction of Ocean-Continent Transition: Constraint from Arc Magmatic Sequence in Kaihua, Western Zhejiang. Earth Science, 45(1): 180-193. doi: 10.3799/dqkx.2018.244

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Neoproterozoic (~800 Ma) Subduction of Ocean-Continent Transition: Constraint from Arc Magmatic Sequence in Kaihua, Western Zhejiang

doi: 10.3799/dqkx.2018.244

1.
Zhejiang Institute of Geological Survey, Hangzhou 311203, China
2.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2018-07-16
Publish Date: 2020-01-15

Abstract

Abstract

As a record of the process for ocean-continent transition related oceanic subduction, the magmatic rocks consisting of the basalts, andesites, dacites and rhyolites, were identified near the northwastern Xiazhuang-Shufan fault in Kaihua County, western Zhejiang, which is the eastern segment of Jiangnan orogeny. Geochemical analyses indicate that the basalts and andesites are mostly enriched in Ba, K, Rb, Th, U, Pb, but depleted in Sr, P, Nb, Ta, Ti. The basalts show high Nb contents of 11.8×10^-6 to 15.2×10^-6, Nb/Ta=15.36-18.10, and Nb/U=8.90-19.32. The andesites have higher Mg values with MgO contents ranging from 5.31% to 8.56%, Mg^# ranging from 56.89 to 68.83, and FeO^T/MgO=0.82-1.36. The dacites and rhyolites have higher Ga/Al ratios, FeO^T/MgO ranging from 5.66 to 18.50 mostly, and high magma temperatures (837-920℃), reflecting the characteristics of A-type rhyolites. The U-Pb dating of zircon yields age of 800.5±9.2 Ma for the Nb-enriched basalt, 799.3±7.1 Ma for the high-Mg andesite, and 798.3±6.2 Ma for the A-type rhyolite, confirming that the magmatic activity of continental marginal arc occurred when the paleo-South-China Plate subducted northwestwardly in Neoproterozoic, and suggesting that the subducting movement continued to 800 Ma or later.
- Nb-enriched basalt,
- high-Mg andesite,
- geochronology,
- geochemistry,
- Neoproterozoic,
- western Zhejiang

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References(95)

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Neoproterozoic (~800 Ma) Subduction of Ocean-Continent Transition: Constraint from Arc Magmatic Sequence in Kaihua, Western Zhejiang

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