广东连山地区禾洞高分异花岗岩的锆石U-Pb年代学及岩石成因

李响; 王令占; 涂兵; 田洋; 谢国刚; 张楗钰; 张宗言

doi:10.3799/dqkx.2021.175

Volume 48 Issue 10

Oct. 2023

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Article Navigation > Earth Science > 2023 > 48(10): 3577-3596

Li Xiang, Wang Lingzhan, Tu Bing, Tian Yang, Xie Guogang, Zhang Jianyu, Zhang Zongyan, 2023. Zircon Geochronology and Petrogenesis of Hedong Highly Fractionated I-Type Granite in Lianshan, Guangdong Province. Earth Science, 48(10): 3577-3596. doi: 10.3799/dqkx.2021.175

Citation:

Li Xiang, Wang Lingzhan, Tu Bing, Tian Yang, Xie Guogang, Zhang Jianyu, Zhang Zongyan, 2023. Zircon Geochronology and Petrogenesis of Hedong Highly Fractionated I-Type Granite in Lianshan, Guangdong Province. Earth Science, 48(10): 3577-3596. doi: 10.3799/dqkx.2021.175

Citation:

Li Xiang, Wang Lingzhan, Tu Bing, Tian Yang, Xie Guogang, Zhang Jianyu, Zhang Zongyan, 2023. Zircon Geochronology and Petrogenesis of Hedong Highly Fractionated I-Type Granite in Lianshan, Guangdong Province. Earth Science, 48(10): 3577-3596. doi: 10.3799/dqkx.2021.175

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Zircon Geochronology and Petrogenesis of Hedong Highly Fractionated I-Type Granite in Lianshan, Guangdong Province

doi: 10.3799/dqkx.2021.175

Li Xiang^{1, 2
,
,},
Wang Lingzhan^{1, 2},
Tu Bing^{1, 2},
Tian Yang^{1, 2},
Xie Guogang¹,
Zhang Jianyu¹,
Zhang Zongyan¹

1.
Wuhan Center of China Geological Survey, Wuhan 430205, China
2.
Research Center of Granitic Diagenesis and Mineralization, China Geological Survey, Wuhan 430205, China

Received Date: 2021-08-08
Available Online: 2023-10-31
Publish Date: 2023-10-25

Abstract

Abstract

The petrogenesis of Late Mesozoic granites in Nanling Mountains region remains controversial. In this paper, it conducts the comprehensive study of petrology, zircon U-Pb chronology, whole-rock element and Sr-Nd-Hf isotopic geochemistry for the Hedong highly fractionated I-type granite in the Lianshan, Guangdong Province. LA-ICP-MS U-Pb zircon analysis yields ²⁰⁶Pb/²³⁸U weighted mean ages of 159.7±1.4 Ma and 160.3±1.7 Ma for the medium-fine-grained biotite syenite granite and medium-grained biotite monzonitic granite respectively, indicating that the pluton was formed in the Late Jurassic. Chemical analyses show that the granite has higher SiO₂ (70.02%-75.56%) and total alkali (7.74%-8.59%), lower TFeO, MgO, CaO, TiO₂, P₂O₅, A/CNK values is ranging from 0.96 to 1.28. The granite is also characterized by higher Rb/Sr ratio (2.6-17.8) and pronounced negative Eu anomalies (δEu ranging from 0.06 to 0.52). The Ga/Al ratio of most granite samples are lower than 2.6, and the Zr+Nb+Ce+Y values are ranging from 118×10^-6 to 313×10^-6, which are lower than the respective values of A-type granites. The granite is also characterized by low zircon saturation temperatures (703-801 ℃). The P₂O₅ contents are negatively correlated with SiO₂ while element Y and Th are positively correlated with Rb. Above geochemical data suggest that the rocks from the Hedong pluton are highly fractional I-type granites. They have relatively low I_Sr values (0.707 00-0.711 39), high ε_Nd(t) values(-7.1 to -2.6)and the ε_Hf(t) values range from -8.4 to +2.2.Their two stage Nd and Hf model ages are 1.30-1.67 Ga and 1.04-1.71 Ga, respectively. Combining with field observation, it suggests that the Hedong pluton was formed by the mixing of crust-derived magmas and mantle-derived magmas. Under the extension environment triggered by subduction of paleo-Pacific plate, the Hedong pluton might form by the underplate of mantle-derived magmas across the Chenzhou-Linwu trans-crustal fault.
- Hedong pluton,
- highly fractionated I-type granite,
- zircon U-Pb chronology,
- Sr-Nd-Hf isotope,
- petrogenesis,
- geochemistry,
- petrology

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References(111)

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Zircon Geochronology and Petrogenesis of Hedong Highly Fractionated I-Type Granite in Lianshan, Guangdong Province

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