东天山地区中天山地块早二叠世后碰撞伸展与壳幔岩浆作用：来自二长闪长玢岩的制约

张维峰; 邓新; 张利国; 王晶; 谢国刚; 金鑫镖

doi:10.3799/dqkx.2023.064

Volume 49 Issue 8

Aug. 2024

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Article Navigation > Earth Science > 2024 > 49(8): 2697-2713

Zhang Weifeng, Deng Xin, Zhang Liguo, Wang Jing, Xie Guogang, Jin Xinbiao, 2024. Early Permian Post-Collisional Extension and Crust-Mantle Magmatism in the Central Tianshan Block, Eastern Tianshan: Constraints from the Study of Porphyritic Monzodiorite. Earth Science, 49(8): 2697-2713. doi: 10.3799/dqkx.2023.064

Citation:

Zhang Weifeng, Deng Xin, Zhang Liguo, Wang Jing, Xie Guogang, Jin Xinbiao, 2024. Early Permian Post-Collisional Extension and Crust-Mantle Magmatism in the Central Tianshan Block, Eastern Tianshan: Constraints from the Study of Porphyritic Monzodiorite. Earth Science, 49(8): 2697-2713. doi: 10.3799/dqkx.2023.064

Citation:

Zhang Weifeng, Deng Xin, Zhang Liguo, Wang Jing, Xie Guogang, Jin Xinbiao, 2024. Early Permian Post-Collisional Extension and Crust-Mantle Magmatism in the Central Tianshan Block, Eastern Tianshan: Constraints from the Study of Porphyritic Monzodiorite. Earth Science, 49(8): 2697-2713. doi: 10.3799/dqkx.2023.064

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Early Permian Post-Collisional Extension and Crust-Mantle Magmatism in the Central Tianshan Block, Eastern Tianshan: Constraints from the Study of Porphyritic Monzodiorite

doi: 10.3799/dqkx.2023.064

Zhang Weifeng^{1, 2
,
,},
Deng Xin^{1
,
,},
Zhang Liguo¹,
Wang Jing¹,
Xie Guogang¹,
Jin Xinbiao¹

1.
Wuhan Center of Geological Survey, Wuhan 430205, China
2.
Research Center for Petrogenesis and Mineralization of Granitoids, Wuhan 430205, China

Received Date: 2023-01-08
Available Online: 2024-08-27
Publish Date: 2024-08-25

Abstract

Abstract

As a typical case of the Permian magmatism in the Eastern Tianshan, the porphyritic monzodiorite exposed in the southern margin of the Central Tianshan block. Zircon U-Pb dating on the monzodiorite yields an age of 281.3±1.5 Ma. The monzodiorite shows high-K calc-alkaline and metaluminous affinities, with Na₂O+K₂O and A/CNK values ranging 5.88‒6.62 wt.% and 0.66‒0.73, respectively. They are characterized by high Fe₂O₃/FeO ratios (0.66~0.73), and present the assemblage of titanite+quartz+magnetite in the groundmass, suggesting that the monzodiorite formed under a high oxygen fugacity condition. The monzodiorite enriched in LILEs (i.e. Rb, K and Ba), but depleted in HFSEs (i.e. Nb, Ta and Ti) and HREE. In addition, all the study samples have negative ε_Nd(t) (-2.72 to -3.07), high initial ⁸⁷Sr/⁸⁶Sr (0.706 46 to 0.706 54) values, and negative zircon ε_Hf(t) (-3.7 to -0.8) values, as well as intermediate Nb/U (10.3 to 10.9) values. These geochemical features indicating that the magmas originated from spinel-garnet lherzolite that metasomatized by subduction-related fluids, and mixed with minor crustal components. Integrating the petrogenesis and other geological evidences, we proposed that the magmatisms in the Central Tianshan block were generated in post-collision extensional setting of slab breakoff during the Early Permian.
- post-collisional extension,
- slab breakoff,
- Permian,
- Petrogenesis,
- Central Tianshan block,
- geochemistry

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References(92)

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