胶-辽-吉活动带中段古元古代早期构造演化：来自牧牛河和大房身岩体的证据

陈志刚; 朱凯; 刘杰勋; 李文庆

doi:10.3799/dqkx.2020.206

Volume 46 Issue 5

May 2021

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Article Navigation > Earth Science > 2021 > 46(5): 1710-1727

Chen Zhigang, Zhu Kai, Liu Jiexun, Li Wenqing, 2021. Early Paleoproterozoic Tectonic Evolution of Central Jiao-Liao-Ji Belt: Evidence from Muniuhe and Dafangshen Plutons. Earth Science, 46(5): 1710-1727. doi: 10.3799/dqkx.2020.206

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Chen Zhigang, Zhu Kai, Liu Jiexun, Li Wenqing, 2021. Early Paleoproterozoic Tectonic Evolution of Central Jiao-Liao-Ji Belt: Evidence from Muniuhe and Dafangshen Plutons. Earth Science, 46(5): 1710-1727. doi: 10.3799/dqkx.2020.206

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Early Paleoproterozoic Tectonic Evolution of Central Jiao-Liao-Ji Belt: Evidence from Muniuhe and Dafangshen Plutons

doi: 10.3799/dqkx.2020.206

Chen Zhigang^{1
,
,},
Zhu Kai^{2
,
,},
Liu Jiexun³,
Li Wenqing⁴

1.
Agency Affairs Bureau of Ministry of Natural Resources, Beijing 100812, China
2.
College of Geo-Exploration Science and Technology, Jilin University, Changchun 130061, China
3.
School of Prospecting and Surveying Engineering, Changchun Institute of Technology, Changchun 130021, China
4.
Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Changchun 130061, China

Received Date: 2020-07-10
Publish Date: 2021-05-15

Abstract

Abstract

Liaoji granitoids are important constituents of the Jiao-Liao-Ji belt (JLJB), and they provide important constraints on tectonic setting of the JLJB. The tectonic setting of the JLJB is still controversial due to the debate on nature of the Liaoji granitoids. It conducted zircon U-Pb geochronological and geochemical analyses of Liaoji granitoids (Muniuhe and Dafangshen plutons) in the Muniuhe-Dafangshen area, and then discuss the petrogenesis and geological significance of these granitoids. LA-ICP-MS U-Pb zircon dating gives the emplacement age of 2 176±4 Ma and 2 179±4 Ma for Muniuhe and Dafangshen plutons, respectively. Muniuhe and Dafangshen granitoids display similar geochemical characteristics. They have high SiO₂ (72.85%-77.67%), alkalis (K₂O+Na₂O=7.65%-8.86%) and K₂O/Na₂O ratios (0.99-1.83), and low CaO (0.10%-0.92%), MgO (0.03%-0.09%) and Al₂O₃ (11.49%-12.67%) contents. The chondrite-normalized REE patterns of Muniuhe and Dafangshen granitoids show right-dipping linear trends with slightly negative Eu anomalies (Eu/Eu^*=0.08-0.56) and high Ga/Al ratios. They are enriched in high field strength elements (HFSEs; e.g., Zr, U and Y) and large-ion lithophile elements (LILEs; e.g., Rb and K), and depleted in Nb, P, Ti and Sr. In addition, they display high Zr saturation temperatures (855-871 ℃ and 850-886 ℃, repectively). Low Nb/Y ratios and high Zr saturation temperatures indicate that the Muniuhe and Dafangshen granitoids have affinities with A₂-subtype granitoids, and they were derived from thinned lower crust. The occurrence of voluminous A₂-subtype granitoids, combined with the newly discovered Na-rich granitoids and calc-alkaline mafic rocks, suggests that the tectonic setting of the JLJB is back-arc basin.
- Jiao-Liao-Ji belt,
- Liaoji granitoids,
- A₂-subtype granitoid,
- back-arc basin,
- tectonics

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Early Paleoproterozoic Tectonic Evolution of Central Jiao-Liao-Ji Belt: Evidence from Muniuhe and Dafangshen Plutons

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