中条山地区涑水杂岩新太古代烟庄正长花岗岩年龄及成因：对华北克拉通地壳演化的制约

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

doi:10.3799/dqkx.2020.254

Volume 45 Issue 9

Sep. 2020

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Article Navigation > Earth Science > 2020 > 45(9): 3161-3178

Yang Chonghui, Du Lilin, Song Huixia, Duan Qingsong, Wang Jianlong, Huang Zhiqiang, Ren Liudong, Geng Yuansheng, Wang Yanbin, 2020. Geochronology and Petrogenesis of Neoarchean Yanzhuang Syenogranites from Sushui Complex in the Zhongtiao Mountains: Implications for the Crustal Evolution of the North China Craton. Earth Science, 45(9): 3161-3178. doi: 10.3799/dqkx.2020.254

Citation:

Yang Chonghui, Du Lilin, Song Huixia, Duan Qingsong, Wang Jianlong, Huang Zhiqiang, Ren Liudong, Geng Yuansheng, Wang Yanbin, 2020. Geochronology and Petrogenesis of Neoarchean Yanzhuang Syenogranites from Sushui Complex in the Zhongtiao Mountains: Implications for the Crustal Evolution of the North China Craton. Earth Science, 45(9): 3161-3178. doi: 10.3799/dqkx.2020.254

Citation:

Yang Chonghui, Du Lilin, Song Huixia, Duan Qingsong, Wang Jianlong, Huang Zhiqiang, Ren Liudong, Geng Yuansheng, Wang Yanbin, 2020. Geochronology and Petrogenesis of Neoarchean Yanzhuang Syenogranites from Sushui Complex in the Zhongtiao Mountains: Implications for the Crustal Evolution of the North China Craton. Earth Science, 45(9): 3161-3178. doi: 10.3799/dqkx.2020.254

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Geochronology and Petrogenesis of Neoarchean Yanzhuang Syenogranites from Sushui Complex in the Zhongtiao Mountains: Implications for the Crustal Evolution of the North China Craton

doi: 10.3799/dqkx.2020.254

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

Received Date: 2020-06-29
Publish Date: 2020-09-15

Abstract

Abstract

The formation of the voluminous syenogranites of the late Neoarchean is an important mark of maturation and stabilization of continental crust, and play a vital role in understanding the formation and evolution of early continental crust. However, the formation age and genesis of the Yanzhuang syenogranite in the Sushui Complex in the southern margin of the North China Craton are not well defined, and the tectonic setting remains controversial. This paper presents the zircon U-Pb ages and Hf isotopes as well as whole rock element and Nd isotope compositions of the Yanzhuang syenogranites. SHRIMP dating of zircon from the granite yields an age of 2 515±7 Ma. The rocks are high in SiO₂ (73.05%－74.85%) and K₂O (4.46%－5.86%) and low in CaO (0.55%－0.98%), total FeO (0.73%－1.28%) and MgO (0.31%－0.52%), with K₂O+Na₂O and A/CNK at 8.32%－9.36% and 1.01－1.04, respectively. They show variations in REE contents (ΣREE=63.8×10^-6－250.02×10^-6), with relative enrichment of LREE to HREE ((La/Yb)_N=25.44－92.87) and somewhat negative Eu anomaly (Eu/Eu^*=0.47－0.79). The rocks are low in Sr and Ba, and high in Rb, Th and U, with depletion in Nb, Zr, Y, Yb, Cr, Co and Ni. Thus they have high Rb/Sr, Rb/Ba and Sr/Yb ratios and low Sm/Nd and Nd/Th ratios, and show the characteristics of highly fractionated I type granite. The Yanzhuang syenogranite has whole-rock ε_Nd(t) values of -1.09－0.89 and magmatic zircon ε_Hf(t) values of 2.85－3.66, with Hf model T_DM2 ages of 2 258－2 883 Ma (mainly 2 600－2 883 Ma). Combined with early work, this study indicates that the Yanzhuang syenogranite shows the feature of syn-collision and post-collision granites formed by partial melting of juvenile crust in a tectonic transition setting from compression to extension, probably with addition of a small amount of mantle material. The formation of voluminous syenogranites in this period marks the termination of the Archean intense magmatism and the stabilization of the North China Craton at the end of the Neoarchean.
- Sushui Complex,
- Yanzhuang syenogranite,
- zircon U-Pb age,
- tectonic setting,
- North China Craton,
- geochemistry

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