扬子陆块北缘西大别地区新元古界定远组双峰式火山岩地球化学特征、成因及其地质意义

朱江; 邱啸飞; 周豹; 张海军; 吴越; 邓新

doi:10.3799/dqkx.2020.229

Volume 46 Issue 4

Apr. 2021

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Article Navigation > Earth Science > 2021 > 46(4): 1311-1327

Zhu Jiang, Qiu Xiaofei, Zhou Bao, Zhang Haijun, Wu Yue, Deng Xin, 2021. Neoproterozoic Bimodal Volcanic Rocks from Dingyuan Formation in Western Dabie Area, Northern Margin of Yangtze Block, China: Geochemistry, Petrogenesis and Geological Implications. Earth Science, 46(4): 1311-1327. doi: 10.3799/dqkx.2020.229

Citation:

Zhu Jiang, Qiu Xiaofei, Zhou Bao, Zhang Haijun, Wu Yue, Deng Xin, 2021. Neoproterozoic Bimodal Volcanic Rocks from Dingyuan Formation in Western Dabie Area, Northern Margin of Yangtze Block, China: Geochemistry, Petrogenesis and Geological Implications. Earth Science, 46(4): 1311-1327. doi: 10.3799/dqkx.2020.229

Citation:

Zhu Jiang, Qiu Xiaofei, Zhou Bao, Zhang Haijun, Wu Yue, Deng Xin, 2021. Neoproterozoic Bimodal Volcanic Rocks from Dingyuan Formation in Western Dabie Area, Northern Margin of Yangtze Block, China: Geochemistry, Petrogenesis and Geological Implications. Earth Science, 46(4): 1311-1327. doi: 10.3799/dqkx.2020.229

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Neoproterozoic Bimodal Volcanic Rocks from Dingyuan Formation in Western Dabie Area, Northern Margin of Yangtze Block, China: Geochemistry, Petrogenesis and Geological Implications

doi: 10.3799/dqkx.2020.229

Zhu Jiang^{1, 2, 3
,
,},
Qiu Xiaofei³,
Zhou Bao⁴,
Zhang Haijun³,
Wu Yue^{1, 2},
Deng Xin³

1.
College of Resources and Environment, Yangtze University, Wuhan 430100, China
2.
Key Laboratory of Exploration Technologies for Oil and Gas Resources, Ministry of Education, Yangtze University, Wuhan 430100, China
3.
Wuhan Center of China Geological Survey, Wuhan 430205, China
4.
Hubei Geological Survey, Wuhan 430034, China

Received Date: 2020-05-26
Publish Date: 2021-04-15

Abstract

Abstract

Neoproterozoic bimodal volcanic rocks from the Dingyuan Formation within the western Dabie terrain consist of rhyolite, rhyolitic tuff and basalt. Elemental, whole-rock Sr-Nd and zircon Hf isotopic analyses were carried out in this study for these volcanic rocks, in order to better understand their petrogenesis and geodynamic processes along the northern margin of Yangtze block. The rhyolite is characterized by high concentrations of SiO₂ and Al₂O₃, belongs to the calc-alkaline series, and is peraluminous. It is enriched in light rare earth elements (LREEs) and shows unapparent Eu anomaly. The basalt has SiO₂ of 48.26% to 51.71%, Mg^# values of 0.32 to 0.59, and is weakly enriched in light rare earth elements. The rhyolite has initial ⁸⁷Sr/⁸⁶Sr ratios ranging from 0.703 5 to 0.707 7, and negative ε_Nd(t) values of -10.6 to -6.5, with calculated two-stage Nd model ages of 1.69 to 2.00 Ga, while the basalt has (⁸⁷Sr/⁸⁶Sr)_i of 0.706 1 to 0.708 1, ε_Nd(t) of -6.6 to +3.4, and the Nd model ages (T_DM) values of 1.44 to 2.02 Ga. In situ zircon Hf isotopic analyses show that the ε_Hf(t) values of zircons from the rhyolite vary from -19.2 to -7.2, with calculated two-stage Hf model ages of 1.77 to 2.59 Ga. The geochemical and Sr-Nd-Hf isotopic signatures suggest that the rhyolite has a close affinity to S-type granite, and is derived from partial melting of the ancient crust of the Yangtze block. The basalt is most likely derived from an enriched lithospheric mantle, with fractional crystallization and assimilation of crustal materials during the evolution of the magma. It is proposed that the Neoproterozoic bimodal volcanic suites from the Dingyuan and the Qijiaoshan formations are erupted coevally, but have different sources and magmatic processes. The bimodal volcanic rocks in this study provide evidences for an enriched lithospheric mantle beneath the Dabie terrain at ca.740 Ma, and a rifting extensional setting for the north margin of the Yangtze block.
- volcanic rock,
- geochemistry,
- petrogenesis,
- Sr-Nd-Hf isotope,
- lithospheric mantle,
- Dabie orogen

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References(71)

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