扬子陆块西南缘早前寒武纪撮科杂岩记录的多期岩浆-变质事件

崔晓庄; 任光明; 孙志明; 王鹏; 刘石磊; 邓奇; 任飞; 庞维华

doi:10.3799/dqkx.2020.199

Volume 45 Issue 8

Aug. 2020

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Article Navigation > Earth Science > 2020 > 45(8): 3054-3069

Cui Xiaozhuang, Ren Guangming, Sun Zhiming, Wang Peng, Liu Shilei, Deng Qi, Ren Fei, Pang Weihua, 2020. Multiple Tectonothermal Events Recorded in the Early Precambrian Cuoke Complex in the Southwestern Yangtze Block, South China. Earth Science, 45(8): 3054-3069. doi: 10.3799/dqkx.2020.199

Citation:

Cui Xiaozhuang, Ren Guangming, Sun Zhiming, Wang Peng, Liu Shilei, Deng Qi, Ren Fei, Pang Weihua, 2020. Multiple Tectonothermal Events Recorded in the Early Precambrian Cuoke Complex in the Southwestern Yangtze Block, South China. Earth Science, 45(8): 3054-3069. doi: 10.3799/dqkx.2020.199

Citation:

Cui Xiaozhuang, Ren Guangming, Sun Zhiming, Wang Peng, Liu Shilei, Deng Qi, Ren Fei, Pang Weihua, 2020. Multiple Tectonothermal Events Recorded in the Early Precambrian Cuoke Complex in the Southwestern Yangtze Block, South China. Earth Science, 45(8): 3054-3069. doi: 10.3799/dqkx.2020.199

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Multiple Tectonothermal Events Recorded in the Early Precambrian Cuoke Complex in the Southwestern Yangtze Block, South China

doi: 10.3799/dqkx.2020.199

Chengdu Center of China Geological Survey, Chengdu 610081, China

Received Date: 2020-06-09
Publish Date: 2020-08-15

Abstract

Abstract

The Cuoke Complex, a newly identified Early Precambrian basement complex in central Yunnan, bears key information for the early evolution of the Yangtze Block. Here, we present zircon U-Pb geochronological and Hf isotopic data of four representative samples collected from this complex. Magmatic zircons of one trondjemitic gneiss sample yield a crystallization age of 2 845±33 Ma, with positive ε_Hf(t) values of 1.7-4.6 and relatively young depleted mantle two stage (T_DM2) model ages of 2.97-3.12 Ga, suggestive of the derivation from remelting of juvenile crust. Meta-monzogranite and gneissic granite yield ages of 2 401±15 Ma and 2 320±16 Ma respectively. They show negative zircon ε_Hf(t) values of -6.2 to -0.8 and older T_DM2 model ages of 2.90-3.11 Ga, indicating that they were formed by remelting of ancient crustal materials. Metamorphic-origin zircons of one plagioclase-biotite cataclasite sample give an age of 1 948±16 Ma. Together with available metamorphic age data, it is revealed that one episode of regional metamorphism occurred at 1.96-1.95 Ga. Our new dataset confirms the existence of Archean basement rocks in the Cuoke Complex. Moreover, multiple magmatic and metamorphic events related to the assembly of the Nuna supercontinent extensively took place in the southwestern Yangtze Block, South China.
- Archean,
- Paleoproterozoic,
- tectonothermal event,
- Cuoke Complex,
- Yangtze Block,
- geochronology

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References(71)

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