大兴安岭北段小柯勒河花岗斑岩脉成因及地质意义:锆石U-Pb年龄、岩石地球化学及Hf同位素制约

doi:10.13278/j.cnki.jjuese.20210073

Abstract

Abstract: In this paper, the granite porphyry geochemistry, zircon U-Pb geochronology and Hf isotopes are studied to discuss the petrogenesis, tectonic setting of the granitic porphyry dike, and the relationship between the rock vein and mineralization of Xiaokelehe. Our data show that the samples are characterized by high content of SiO₂(69.85%-70.48%) and alkali (9.74%-9.89%), and low content of MgO (0.34%-0.40%) and CaO (1.04%-1.20%). The A/CNK values range from 0.98 to 1.02, the granitic porphyry is quasi-aluminum-weak per-aluminum. The rock is rich in LREE and poor in HREE, with obviously negative Eu anomalies. They are rich in LILEs (Rb and K) and HFSEs (Th, U, Hf, and Zr), and depleted of LILEs (Srand Ba) and HFSEs (Nb, Ta, Ti, and P). The samples have 10⁴Ga/Al values ranging from 2.32 to 3.68 and I_D values ranging from 87.63 to 89.01. All these characteristics indicate that the granite porphyry is fractionated I-type granite. The zircon U-Pb dating indicates that the rock was formed in the Early Cretaceous ((124.0±0.6) Ma). The Hf isotope results show that the ε_Hf (t) values of the granite porphyry range from 0.5 to 3.3, and two-stage Hf model ages (T_DM2) range from 1 150 to 970 Ma, which indicates that the magma originated from the partial melting of Meso-Neoproterozoic juvenile crust that was derived from the depleted mantle, and there was a small amount of ancient crust added. The granite porphyry was formed in the extensional environment under the background of the Mongolia-Okhotsk closure in the Late Early Cretaceous. At that time, the Paleo-Pacific plate continued to subduct toward the Eurasian continent, but its influence on this area was limited.

Key words: I-type granite, petrogeochemistry, zircon U-Pb geochronology, Hf isotopes, Da Hinggan Mountains

CLC Number:

P581

Gong Yundi, Li Bile, Li Zhihua, Yu Runtao, Sun Yonggang, Zhang Sen. Petrogenesis and Geological Significance of Granite Porphyry Dike from Xiaokelehe in North Da Hinggan Mountains: Constraints from Zircon U-Pb Age, Geochemistry and Hf Isotopic Composition[J].Journal of Jilin University(Earth Science Edition), 2021, 51(6): 1753-1769.

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Petrogenesis and Geological Significance of Granite Porphyry Dike from Xiaokelehe in North Da Hinggan Mountains: Constraints from Zircon U-Pb Age, Geochemistry and Hf Isotopic Composition

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