| Citation: |
JIAO Dongchen, QU Junfeng. 2024. Warm subduction origin of 2.5 Ga TTG in Zhongtiao Mountains, Shanxi: Constraints from phase equilibrium modeling. Geological Bulletin of China, 43(12): 2272-2287. doi: 10.12097/gbc.2024.08.005
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Warm subduction origin of 2.5 Ga TTG in Zhongtiao Mountains, Shanxi: Constraints from phase equilibrium modeling
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Abstract
The tectonic transition that occurred around 2.5 Ga represents one of the most significant geological events in Earth's history, shaping the early processes of continental growth and cratonization. As the dominant component of the Archean continental crust, TTGs provide valuable insights into the dynamic mechanisms of Archean plate tectonics. However, the lack of data on the pressure−temperature (P−T) conditions during the water−bearing melting processes of TTGs limits our ability to fully identify the tectonic mechanisms involved. This study investigates the 2.5 Ga TTGs in the Zhongtiao Mountains, using 2.5 Ga metabasalt from Wenjiapo as the source rock. Quantitative forward modeling of TTG magmatism revealed that 25% water−bearing melting at a geothermal gradient of 900℃/GPa satisfies the conditions for the formation of the 2.5 Ga TTGs in the Zhongtiao Mountains. The findings suggest that these TTGs formed in a warm subduction environment, indicating that by 2.5 Ga, the North China Craton had already developed a horizontal growth mechanism, consistent with global plate growth events. Additionally, anomalies in certain geochemical indicators suggest that the tectonic mechanism was beginning to transition toward a modern plate subduction environment.
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References
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JIAO Dongchen, QU Junfeng. 2024. Warm subduction origin of 2.5 Ga TTG in Zhongtiao Mountains, Shanxi: Constraints from phase equilibrium modeling. Geological Bulletin of China, 43(12): 2272-2287. doi: 10.12097/gbc.2024.08.005
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Figure 1.
Simplified geological map showing the distribution of metamorphic complexes in the NCC
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Figure 2.
Geological map of the Zhongtiao Mountain region
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Figure 3.
Regional geological map of the Xiaxian in Zhongtiao Mountain, Shanxi Province
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Figure 4.
Simplified P-T phase diagram for an average of Wenjiapo amphibolite
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Figure 5.
Calculated composition of melt produced from the average of Wenjiapo amphibolite at various melt fractions, normalized to the average of 2.5 Ga Sushui TTG gneiss
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Figure 6.
The relationship between minerals, melts proportions, and temperature of Wenjiapo metamorphic basalt at different degrees of melting
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Figure 7.
Comparison of trace elements in Wenjiapo metamorphic basalt and TTG at different degrees of melting
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Figure 8.
Late Neoarchean tectonic model for the Southern North China Craton (ca. 2.5 Ga)