吉林通化赤柏松地区早白垩世花岗质岩脉（株）的成因：锆石U-Pb年代学、Hf同位素和地球化学证据

周皓; 裴福萍; 焦骥; 王枫; 许文良

doi:10.3799/dqkx.2018.309

Volume 45 Issue 2

Feb. 2020

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Zhou Hao, Pei Fuping, Jiao Ji, Wang Feng, Xu Wenliang, 2020. Petrogenesis of Early Cretaceous Chibaisong Granitoid Dyke (Stock) from Tonghua Area, Jilin Province: Evidences from Zircon U-Pb Geochronology, Hf Isotope and Whole-Rock Geochemistry. Earth Science, 45(2): 519-533. doi: 10.3799/dqkx.2018.309

Citation:

Zhou Hao, Pei Fuping, Jiao Ji, Wang Feng, Xu Wenliang, 2020. Petrogenesis of Early Cretaceous Chibaisong Granitoid Dyke (Stock) from Tonghua Area, Jilin Province: Evidences from Zircon U-Pb Geochronology, Hf Isotope and Whole-Rock Geochemistry. Earth Science, 45(2): 519-533. doi: 10.3799/dqkx.2018.309

Citation:

Zhou Hao, Pei Fuping, Jiao Ji, Wang Feng, Xu Wenliang, 2020. Petrogenesis of Early Cretaceous Chibaisong Granitoid Dyke (Stock) from Tonghua Area, Jilin Province: Evidences from Zircon U-Pb Geochronology, Hf Isotope and Whole-Rock Geochemistry. Earth Science, 45(2): 519-533. doi: 10.3799/dqkx.2018.309

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Petrogenesis of Early Cretaceous Chibaisong Granitoid Dyke (Stock) from Tonghua Area, Jilin Province: Evidences from Zircon U-Pb Geochronology, Hf Isotope and Whole-Rock Geochemistry

doi: 10.3799/dqkx.2018.309

College of Earth Sciences, Jilin University, Changchun 130061, China

Received Date: 2018-12-30
Publish Date: 2020-02-15

Abstract

Abstract

LA-ICP-MS zircon U-Pb geochronology, whole-rock geochemistry and Hf isotope of zircons of Early Cretaceous Chibaisong granitoids in Tonghua area, southern Jilin Province, northeast (NE) China provide the insights into the nature of the lower crust and tectonic evolution of the eastern North China Craton (NCC). Zircons from the Chibaisong granitoid dyke (stock) show fine-scale oscillatory zoning, and relatively high Th/U ratios (0.53~1.94), indicative a magmatic origin. The weighted mean of ²⁰⁶Pb/²³⁸U ages for four samples from four granitoids are 116 Ma, 124 Ma, 127 Ma and 130 Ma, respectively. The Chibaisong granitoids have variable content of SiO₂ (60.61%-76.07%) and MgO (0.01%-2.48%), high content of total-alkali (K₂O+Na₂O=6.26%-9.14%) and Al₂O₃ (11.99%-16.13%), characterized by the nature of high-K calc-alkaline series.Additionally, they show enrichment of LREEs and LILEs, depletion of HREEs and HFSEs, Ba, Sr, P, Ti and Eu (Eu/Eu^*=0.05-0.30), suggesting that they were derived from the partial melting of the lower crust, and suffered from the fractional crystallization of plagioclase, alkali feldspar, apatite and ilmenite. Furthermore, they were assimilated by the country rock according to their variable major element contents and zircon ε_Hf(t)values. Granitoids were more alkaline in the early stage of the Early Cretaceous and Mg^# was increased, which may be attributed to mantle material. The zircon ε_Hf(t) values in the samples ranged from -21.84 to -10.74, and the two-stage model ages of zircon Hf isotope of granite porphyry yield 1.86-2.56 Ga, which imply that the accretion of the lower crust within the Tonghua area mainly happened in the Paleoproterozoic, with small amounts during Neoproterozoic. The bimodal rock associationin the Early Cretaceous, together with the results from the contemporaneous volcanic rocks and regional evolution history in this area, indicate that the granitoid dykes may formed in an extensional setting, and more strongly extension happened during the late stage of Early Cretaceous associated with the subduction of the Paleo-Pacific Plate beneath the Eurasian continent.
- Early Cretaceous,
- Chibaisong,
- granitoid dyke (stock),
- geochemistry,
- zircon Hf isotope

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