塔里木新元古代裂谷盆地基底结构与演化

陈利新; 贾承造; 邬光辉; 黄少英; 杨率; 陈永权; 苏洲

doi:10.3799/dqkx.2023.150

Volume 49 Issue 10

Oct. 2024

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Article Navigation > Earth Science > 2024 > 49(10): 3445-3458

Chen Lixin, Jia Chengzao, Wu Guanghui, Huang Shaoying, Yang Shuai, Chen Yongquan, Su Zhou, 2024. Basement Architecture and Evolution of Neoproterozoic Tarim Rift Basin. Earth Science, 49(10): 3445-3458. doi: 10.3799/dqkx.2023.150

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Chen Lixin, Jia Chengzao, Wu Guanghui, Huang Shaoying, Yang Shuai, Chen Yongquan, Su Zhou, 2024. Basement Architecture and Evolution of Neoproterozoic Tarim Rift Basin. Earth Science, 49(10): 3445-3458. doi: 10.3799/dqkx.2023.150

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Basement Architecture and Evolution of Neoproterozoic Tarim Rift Basin

doi: 10.3799/dqkx.2023.150

1.
Unconventional Gas Research Institute, China Petroleum University, Beijing 102249, China
2.
PetroChina Tarim Oilfield Company, Korla 841000, China
3.
School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China

Received Date: 2023-01-17
Available Online: 2024-11-08
Publish Date: 2024-10-25

Abstract

Abstract

The basement architecture and evolution is of important role in dechipering sedimentary basin dynamitics.Based on the compiled geochronological and geochemical data, it has a review on the hot debates on the basement architecture, tectonic environment and evolution of the Neoproterozoic Tarim Basin.The results show that the southern and northern Tarim terranes are assemblied during 1.9-1.8 Ga, and the Early Neoproterozoic sedimentary succession and Paleoproterozoic igneous succession are composed to form a unified metamorphic basement during 780-750 Ma, and to form a complex metamorphic basement structure with differences between northern and southern terranes by multi-stage tectonic-thermal events. The Neoproterozoic was characterized by multi-stage of advancing subduction at ca. 950-900 Ma, 860-840 Ma, 830-800 Ma, 780-760 Ma, and multi-stages of retreating subduction at ca. 760-720 Ma, 670-610 Ma, which resulting in a Neoproterozoic advancing-retreating subduction cycle with the switch at ca. 760 Ma. The Neoproterozoic advancing subduction controlled the origin and evolution of the metamorphic basement, and the subsequent retreating subduction controlled the initiation and evolution of continental rift basin, which suggests a different basin dynamic mechanism and evolutionary process from the classical Wilson cycle.
- Tarim,
- Neoproterozoic,
- basement architecture,
- subduction mechanism,
- rift basin,
- evolution,
- structural geology

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References

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Basement Architecture and Evolution of Neoproterozoic Tarim Rift Basin

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