大兴安岭北段中—新生代玄武岩成分变异:对地幔热演化过程意义

唐杰; 许文良; 李宇; 孙晨阳

doi:10.3799/dqkx.2019.055

Volume 44 Issue 4

Apr. 2019

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Tang Jie, Xu Wenliang, Li Yu, Sun Chenyang, 2019. Composition Variations of Mesozoic and Cenozoic Basalts in Northern Great Xing'an Range: Implications for Thermal Evolution of Mantle. Earth Science, 44(4): 1096-1112. doi: 10.3799/dqkx.2019.055

Citation:

Tang Jie, Xu Wenliang, Li Yu, Sun Chenyang, 2019. Composition Variations of Mesozoic and Cenozoic Basalts in Northern Great Xing'an Range: Implications for Thermal Evolution of Mantle. Earth Science, 44(4): 1096-1112. doi: 10.3799/dqkx.2019.055

Citation:

Tang Jie, Xu Wenliang, Li Yu, Sun Chenyang, 2019. Composition Variations of Mesozoic and Cenozoic Basalts in Northern Great Xing'an Range: Implications for Thermal Evolution of Mantle. Earth Science, 44(4): 1096-1112. doi: 10.3799/dqkx.2019.055

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Composition Variations of Mesozoic and Cenozoic Basalts in Northern Great Xing'an Range: Implications for Thermal Evolution of Mantle

doi: 10.3799/dqkx.2019.055

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources of China, Changchun 130061, China
3.
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

Received Date: 2019-01-14
Publish Date: 2019-04-15

Abstract

Abstract

Recently, few researches have been made on the thermal evolution of the mantle in Northeast China. An effective means to solve this issue is to study the variation characteristics in composition of basalts in Northeast China. In this paper, it summarizes and discusses the composition variations of the Mesozoic and Cenozoic basalts in the northern Great Xing'an Range, with the aim of revealing the thermal evolution of the mantle within the study area. The Early Cretaceous basalts in the northern Great Xing'an Range geochemically belong to tholeiitic series, which are characterized by depletion in high field strength elements (e.g., Nb, Ta and Ti).Their La/Nb and La/Ta ratios range from 1.8 to 5.6 and from 30 to 87, respectively, implying the basaltic magmas originated from the partial melting of the lithospheric mantle. Their initial ⁸⁷Sr/⁸⁶Sr ratios of 0.704 5-0.706 9, ε_Nd(t) values of -1.52-+3.60 and ε_Hf(t) values of +1.74-+7.77 further indicate that the magma source is weakly depleted-weakly enriched lithospheric mantle. Additionally, the Sr-Nd-Pb isotope compositions of the Early Cretaceous basalts suggest that their magmatic sources are characterized by mixing between DM and EMⅡ modified by subduction-derived fluids.Taking the above-mentioned into consideration, it is suggested that the Early Cretaceous basaltic magma was derived from partial melting of a lithospheric mantle metasomated by subduction-related fluids.The Cenozoic ultrapotassic and potassic basalts have weakly negative Nb-Ta anomalies, ⁸⁷Sr/⁸⁶Sr ratios of 0.704 7-0.705 7 and ε_Nd(t) values of -6.3 to -0.8 whereas the mantle xenoliths entrained by Cenozoic ultrapotassic and potassic basalts show the depleted Sr-Nd isotopic characteristics. The Cenozoic sodium basalts have positive Nb-Ta anomalies, and lower ⁸⁷Sr/⁸⁶Sr ratios of 0.703 5-0.704 2 and higher ε_Nd(t) values of +3.4-+6.6 than those of the ultrapotassic and potassic basalts, similar to those of MORB. These geochemical features suggest that the Cenozoic basaltic magmas in the northern Great Xing'an Range were primarily produced by melting of asthenospheric mantle. The composition variations of the Early Cretaceous and Cenozoic basalts in the northern Great Xing'an Range not only indicate that the basaltic magma sources had changed from lithospheric to asthenospheric mantle, but also reveal the thermal evolution of the mantle in the study area, i.e., high geothermal gradient in the late Early Cretaceous changed to low geothermal gradient in the Cenozoic. Combined with the regional tectonic evolution, it is concluded that the Early Cretaceous basaltic magmatism in the northern Great Xing'an Range is related to the taphrogeny caused by the lithospheric extension and thinning, while the Cenozoic basaltic magmatism is related to the intracontinental rifting.
- northern Great Xing'an Range,
- Early Cretaceous,
- Cenozoic,
- basalts,
- thermal evolution of the mantle,
- petrology

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References(127)

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Composition Variations of Mesozoic and Cenozoic Basalts in Northern Great Xing'an Range: Implications for Thermal Evolution of Mantle

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