古元古代全球静寂期岩浆活动——以华北克拉通南缘中条山~2.3 Ga横岭关花岗岩为例

段庆松; 宋会侠; 杜利林; 任留东; 耿元生; 王建龙; 黄智强; 王彦斌; 杨崇辉

doi:10.3799/dqkx.2020.237

Volume 45 Issue 9

Sep. 2020

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Article Navigation > Earth Science > 2020 > 45(9): 3372-3385

Duan Qingsong, Song Huixia, Du Lilin, Ren Liudong, Geng Yuansheng, Wang Jianlong, Huang Zhiqiang, Wang Yanbin, Yang Chonghui, 2020. The Magmatic Activity in Paleoproterozoic Global Magmatic Quiescence: Take the ~2.3 Ga Henglingguan Granites from Zhongtiao Mountains in the Southern North China Craton as an Example. Earth Science, 45(9): 3372-3385. doi: 10.3799/dqkx.2020.237

Citation:

Duan Qingsong, Song Huixia, Du Lilin, Ren Liudong, Geng Yuansheng, Wang Jianlong, Huang Zhiqiang, Wang Yanbin, Yang Chonghui, 2020. The Magmatic Activity in Paleoproterozoic Global Magmatic Quiescence: Take the ~2.3 Ga Henglingguan Granites from Zhongtiao Mountains in the Southern North China Craton as an Example. Earth Science, 45(9): 3372-3385. doi: 10.3799/dqkx.2020.237

Citation:

Duan Qingsong, Song Huixia, Du Lilin, Ren Liudong, Geng Yuansheng, Wang Jianlong, Huang Zhiqiang, Wang Yanbin, Yang Chonghui, 2020. The Magmatic Activity in Paleoproterozoic Global Magmatic Quiescence: Take the ~2.3 Ga Henglingguan Granites from Zhongtiao Mountains in the Southern North China Craton as an Example. Earth Science, 45(9): 3372-3385. doi: 10.3799/dqkx.2020.237

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The Magmatic Activity in Paleoproterozoic Global Magmatic Quiescence: Take the ~2.3 Ga Henglingguan Granites from Zhongtiao Mountains in the Southern North China Craton as an Example

doi: 10.3799/dqkx.2020.237

Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2020-06-20
Publish Date: 2020-09-15

Abstract

Abstract

A large number of ~2.3 Ga geologic bodies have been identified in the North China Craton (NCC) in global magmatic quiescence, which is vital for unveiling the Paleoproterozoic geological evolution on the NCC. This paper presents the whole rock geochemical data, zircon U-Pb ages and Hf isotopes of the Henglingguan monzogranite in Zhongtiao mountains area. LA-ICPMS dating of zircon from the Henglingguan monzogranite yields an age of 2 308±12 Ma. The Henglingguan monzogranite is high in SiO₂, K₂O, Al₂O₃ and alkali, and low in CaO, NaO and TiO₂, with A/CNK concentrated between 1.0 and 1.1, which belongs to high-K calc-alkaline and metaluminous-peraluminous series. The monzogranite is high in total REE contents, showing strong fractionation of LREE and HREE and obvious negative Eu anomaly. As to the trace elements, the monzogranite shows enrichment in Nb, Ta, Zr, Hf, U and Rb, and depletion in V, Cr, Co and Ni, which is consistent with characteristics of I-type granite. Zircons in the Henglingguan monzogranite have ε_Hf(t) values ranging from 0.52 to 6.24, with an average of 2.06, and Hf model T_DM1 age of 2 419-2 642 Ma and T_DM2 age of 2 438-2 738 Ma. The Henglingguan monzogranite shows the features of syn-collision granites originated from partial melting of the ~2.5 Ga ancient crust in collision environment, which shows the NCC was not quiet during the Paleoproterozoic global magmatic quiescence.
- Zhongtiao mountains,
- Henglingguan monzogranite,
- Paleoproterozoic magmatic quiescence,
- tectonic setting,
- geochemistry

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References(111)

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