内蒙古迪彦庙孬来可图侵入岩的年代学、Sr-Nd-Hf同位素特征及其地质意义

范玉须; 肖庆辉; 程杨; 李岩; 刘勇; 郭灵俊; 庞进力

doi:10.3799/dqkx.2020.100

Volume 45 Issue 7

Jul. 2020

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Article Navigation > Earth Science > 2020 > 45(7): 2379-2392

Fan Yuxu, Xiao Qinghui, Cheng Yang, Li Yan, Liu Yong, Guo Lingjun, Pang Jinli, 2020. Chronology, Sr-Nd-Hf Isotope Geochemistry and Geology Significance of Pluton in the Naolaiketu of Diyanmiao, Inner Mongolia. Earth Science, 45(7): 2379-2392. doi: 10.3799/dqkx.2020.100

Citation:

Fan Yuxu, Xiao Qinghui, Cheng Yang, Li Yan, Liu Yong, Guo Lingjun, Pang Jinli, 2020. Chronology, Sr-Nd-Hf Isotope Geochemistry and Geology Significance of Pluton in the Naolaiketu of Diyanmiao, Inner Mongolia. Earth Science, 45(7): 2379-2392. doi: 10.3799/dqkx.2020.100

Citation:

Fan Yuxu, Xiao Qinghui, Cheng Yang, Li Yan, Liu Yong, Guo Lingjun, Pang Jinli, 2020. Chronology, Sr-Nd-Hf Isotope Geochemistry and Geology Significance of Pluton in the Naolaiketu of Diyanmiao, Inner Mongolia. Earth Science, 45(7): 2379-2392. doi: 10.3799/dqkx.2020.100

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Chronology, Sr-Nd-Hf Isotope Geochemistry and Geology Significance of Pluton in the Naolaiketu of Diyanmiao, Inner Mongolia

doi: 10.3799/dqkx.2020.100

Fan Yuxu^{1, 2
,
,},
Xiao Qinghui^{2
,
,
,},
Cheng Yang³,
Li Yan³,
Liu Yong²,
Guo Lingjun⁴,
Pang Jinli⁴

1.
General Prospecting Institute China National Administration of Coal Geology, Beijing 100039, China
2.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
Institute of Mineral Resources, China Metallurgical Geology Administration, Beijing 101300, China
4.
Geological Survey Institute of Inner Mongolia, Hohhot 010020, China

Received Date: 2020-04-29
Publish Date: 2020-07-15

Abstract

Abstract

In this study, we carried out zircon LA-ICP-MS U-Pb geochronology, Sr-Nd-Hf isotope geochemistry on the Naolaiketu tonalite to discuss its origin and tectonic setting. The zircon U-Pb age of the rock is 322.2±1.3 Ma, which indicates that the pluton is a product of the Early Carboniferous magmatic event. Geochemically, the tonalite samples are characterized by moderate-high concentrations of SiO₂(62.29%-77.17%), low Al₂O₃ (11.45%-14.11%) and rich in Na₂O and poor in K₂O, and are enriched in LILE and depleted in HFSE, which show the geochemical characteristics of TTG. The fractionation of LREE and HREE are not obvious, and there arenegative Eu anomaly (δEu=0.64-0.76). The (⁸⁷Sr/⁸⁶Sr)_i of the rocks are low (0.703 457-0.703 789), ε_Nd(t) are all positive (+8.4 to +9.3).The in-situ zircon Hf isotopic analysis show depleted compositions, and ε_Hf(t) range from +8.1 to +13.3, imply that the magma originated from the subducted oceanic crust. Combined with the analysis of regional geological background, the TTG magma event in Naolaiketu indicates that, the palo-Asian Ocean was not closed in the Carboniferous in the Diyanmiao area of West Ujimqin, and the subduction zone was a thermal structure of warm crust-mantle.
- the palo-Asian ocean,
- TTG,
- zircon chronology,
- Sr-Nd isotope,
- subduction plate,
- geochemistry

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References(94)

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Chronology, Sr-Nd-Hf Isotope Geochemistry and Geology Significance of Pluton in the Naolaiketu of Diyanmiao, Inner Mongolia

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