南岭金鸡岭岩体锆石U-Pb年龄、地球化学特征及地质意义

李剑锋; 付建明; 马昌前; 卢友月; 程顺波; 马丽艳; 秦拯纬; 盛海琴

doi:10.3799/dqkx.2020.170

Volume 46 Issue 4

Apr. 2021

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Article Navigation > Earth Science > 2021 > 46(4): 1231-1247

Li Jianfeng, Fu Jianming, Ma Changqian, Lu Youyue, Cheng Shunbo, Ma Liyan, Qin Zhengwei, Sheng Haiqin, 2021. Zircon U-Pb Ages, Geochemical Characteristics and Geological Significance of Jinjiling Pluton in Nanling. Earth Science, 46(4): 1231-1247. doi: 10.3799/dqkx.2020.170

Citation:

Li Jianfeng, Fu Jianming, Ma Changqian, Lu Youyue, Cheng Shunbo, Ma Liyan, Qin Zhengwei, Sheng Haiqin, 2021. Zircon U-Pb Ages, Geochemical Characteristics and Geological Significance of Jinjiling Pluton in Nanling. Earth Science, 46(4): 1231-1247. doi: 10.3799/dqkx.2020.170

Citation:

Li Jianfeng, Fu Jianming, Ma Changqian, Lu Youyue, Cheng Shunbo, Ma Liyan, Qin Zhengwei, Sheng Haiqin, 2021. Zircon U-Pb Ages, Geochemical Characteristics and Geological Significance of Jinjiling Pluton in Nanling. Earth Science, 46(4): 1231-1247. doi: 10.3799/dqkx.2020.170

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Zircon U-Pb Ages, Geochemical Characteristics and Geological Significance of Jinjiling Pluton in Nanling

doi: 10.3799/dqkx.2020.170

1.
Wuhan Center of China Geological Survey, Wuhan 430205, China
2.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
School of Geography, Liaoning Normal University, Dalian 116029, China

Received Date: 2020-05-06
Publish Date: 2021-04-15

Abstract

Abstract

A study of LA-ICP-MS zircon U-Pb dating for Jinjiling pluton from Jiuyishan area in Nanling granite belt was carried out. The results show that the diagenetic age of the main medium grained porphyritic syenite and the complement fine-grained porphyritic monzonite are 156.40±0.66 Ma and 153.00±2.20 Ma, respectively. Combined with the existing data, their ages are restricted between (156.40±0.66)-(159.00±0.45) Ma and (146.00±0.86)-(153.00±2.20) Ma, which indicates that the Jinjiling pluton was formed during the early Yanshanian. Geochemical data show that the Jinjiling pluton is characterized by enriched silicone-alkali, depleted calcium-magnesium and metal uminous-peraluminous (A/KNC=0.97-1.14). The content of rare earth elements of the main granite are significantly higher than those of the complement granites, which is 488.63×10^-6-571.67×10^-6and 166.33×10^-6-275.51×10^-6, respectively. The main granite is enriched in light rare earth elements (LREE), with the complement granite having no obvious fractionation, both of which show negative Eu anomalies and (La/Yb)_N values ranging from 10.27 to 15.84 and 0.38 to 1.13, respectively. The differentiation index (DI) are 88.76-89.20, 90.66-94.06, which indicate that the complement granite has undergone stronger magmatic differentiation. The Jinjiling pluton is enriched in large ion lithophile elements (LILE, e.g., Rb, K, Th, U, Nd and Hf) and relatively depleted in high field strength elements (HFSEs, e.g., Ba, Sr, P, Nb and Ti), with Ga/Al(10⁴) ratios of 3.32-5.02 (average 3.50), Zr+Nb+Ce+Y of 255.5×10^-6-554.9×10^-6(average 422.37×10^-6) and zircon saturation temperatures T_Zr of 780.31-820.67℃ (average 803.77℃), similar to geochemical features of A-type granites. The Jinjiling pluton has higher initial Sr isotope values of 0.712 58 to 0.732 51, lower ε_Nd(t) values of -6.2 to -7.0 and ε_Hf(t) values of -4.2 to -5.5, revealing that the source area of the Jinjiling pluton is mainly composed of crustal materials, without any contributions from mantle or new continental crust materials. The model ages of Nd and Hf are relatively close, with 1 465-1 566 Ma and 1 459-1 541 Ma, respectively, suggesting that the source rocks were separated from the mantle reservoir during the Mesoproterozoic. Combined with the geological evolution of Nanling area, it is inferred that the tectonic background of Jinjiling pluton is an intracontinental extensional environment caused by subduction of Pacific plate.
- A-type granite,
- zircon U-Pb dating,
- isotope geochemistry,
- tectonics,
- Jinjiling,
- Nanling

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Zircon U-Pb Ages, Geochemical Characteristics and Geological Significance of Jinjiling Pluton in Nanling

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