兴蒙造山带中段锡林浩特跃进地区石炭纪岛弧型侵入岩:年代学、地球化学、Sr-Nd-Hf同位素特征及其地质意义

王树庆; 胡晓佳; 杨泽黎; 赵华雷; 张永; 郝爽; 何丽

doi:10.3799/dqkx.2017.510

Volume 43 Issue 3

Mar. 2018

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Wang Shuqing, Hu Xiaojia, Yang Zeli, Zhao Hualei, Zhang Yong, Hao Shuang, He Li, 2018. Geochronology, Geochemistry, Sr-Nd-Hf Isotopic Characteristics and Geological Significance of Carboniferous Yuejin Arc Intrusive Rocks of Xilinhot, Inner Mongolia. Earth Science, 43(3): 672-695. doi: 10.3799/dqkx.2017.510

Citation:

Wang Shuqing, Hu Xiaojia, Yang Zeli, Zhao Hualei, Zhang Yong, Hao Shuang, He Li, 2018. Geochronology, Geochemistry, Sr-Nd-Hf Isotopic Characteristics and Geological Significance of Carboniferous Yuejin Arc Intrusive Rocks of Xilinhot, Inner Mongolia. Earth Science, 43(3): 672-695. doi: 10.3799/dqkx.2017.510

Citation:

Wang Shuqing, Hu Xiaojia, Yang Zeli, Zhao Hualei, Zhang Yong, Hao Shuang, He Li, 2018. Geochronology, Geochemistry, Sr-Nd-Hf Isotopic Characteristics and Geological Significance of Carboniferous Yuejin Arc Intrusive Rocks of Xilinhot, Inner Mongolia. Earth Science, 43(3): 672-695. doi: 10.3799/dqkx.2017.510

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Geochronology, Geochemistry, Sr-Nd-Hf Isotopic Characteristics and Geological Significance of Carboniferous Yuejin Arc Intrusive Rocks of Xilinhot, Inner Mongolia

doi: 10.3799/dqkx.2017.510

1.
Tianjin Institute of Geology and Mineral Resources, China Geological Survey, Tianjin 300170, China
2.
Regional Geology and Mineral Resources Survey Institute of Hebei Province, Langfang 065000, China

Received Date: 2017-10-19
Publish Date: 2018-03-15

Abstract

Abstract

The study of magmatism can reveal the structure and tectonic evolution of the orogeny. In this paper, we present zircon LA-MC-ICP-MS U-Pb dating, Hf-Sr-Nd isotopic compositions and whole rock geochemical data of the Carboniferous Arc intrusive rocks from Yuejin region of Xilinhot, central part of the Xingmeng Orogenic Belt. The rock suit consists of three major rock types, i.e., granodiorite, tonalite and quartz-diorite, with zircon U-Pb ages ranging from 310±1 to 330±1 Ma. Geochemically, these rocks show moderate SiO₂, high and variable Na₂O, Al₂O₃, and CaO contents, but low K₂O, FeO_t and MgO contents.The Na₂O/K₂O ratios are all higher than 1(1.05-2.68, average of 1.95), while these rocks are of Calc-Alkaline series. The A/CNK ratios range from 0.86 to 1.17, indicating most of samples are meta-to weak per-aluminous series. The Mg^# are moderately high, from 47.5-55.8. The trace elemental data of these rocks display enrichment of LILEs, such as Rb, Ba, Th, U, K, but depletion of HFSE, i.e., Nb, Ta, P and Ti. The total REE contents are low (3.62×10^-6-172.33×10^-6, average of 118.33×10^-6) with moderate fractionation between LREE and HREE ((La/Yb)_N range from 2.48-9.44), while weak negative Eu abnormity are observed(δEu range from 0.70 to 1.04). The in-situ zircon Hf isotopic analysis show depleted compositions with ¹⁷⁶Hf/¹⁷⁷Hf ratios varying from 0.282 723 to 0.282 863, ε_Hf(t) values from +2 to +9.9 and Hf two stage model ages(T_DM^C) from 829 to 1 536 Ma(concentrating from 900 to 1 200 Ma). The whole rock Sr-Nd isotopic analysis of (⁸⁷Sr/⁸⁶Sr)_i range from 0.703 7 to 0.704 8, (¹⁴³Nd/¹⁴⁴Nd)_i range from 0.512 320 to 0.512 401, with positive ε_Nd(t) (+2.1 to +3.6), indicating depleted source, and the Nd two stage model ages(T_DM2) are of Neoproterozoic(793-918 Ma). The rock suit, whole rock geochemistry, Hf-Sr-Nd isotopic characteristics indicate that Yuejin Carboniferous intrusive rocks were formed in active continental margin, by the partial melting of basic juvenile crust (formed in Late Mesoproterozoic to Early Neoproterozoic) triggered by subduction fluid and arc basic magma. This tectonic setting demonstrates that there was still subduction in Carboniferous in Xingmeng orogeny and the ocean was not closed.
- Carboniferous,
- arc intrusive rocks,
- active continental margin,
- Xingmeng orogeny,
- subduction,
- juvenile crust

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