赣西北蒙山地区三叠纪挤压‒伸展构造体制转换及其对硅灰石矿的控矿意义

赵东安; 王国灿; 王先广; 胡正华; 刘少华; 申添毅; 朱能杰

doi:10.3799/dqkx.2022.500

Volume 48 Issue 11

Nov. 2023

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Article Navigation > Earth Science > 2023 > 48(11): 4053-4071

Zhao Dongan, Wang Guocan, Wang Xianguang, Hu Zhenghua, Liu Shaohua, Shen Tianyi, Zhu Nengjie, 2023. Triassic Compressional-Extensional Transition in Mengshan Area, NW Jiangxi Province, and Its Ore-Controlling Significance for Wollastonite Deposit. Earth Science, 48(11): 4053-4071. doi: 10.3799/dqkx.2022.500

Citation:

Zhao Dongan, Wang Guocan, Wang Xianguang, Hu Zhenghua, Liu Shaohua, Shen Tianyi, Zhu Nengjie, 2023. Triassic Compressional-Extensional Transition in Mengshan Area, NW Jiangxi Province, and Its Ore-Controlling Significance for Wollastonite Deposit. Earth Science, 48(11): 4053-4071. doi: 10.3799/dqkx.2022.500

Citation:

Zhao Dongan, Wang Guocan, Wang Xianguang, Hu Zhenghua, Liu Shaohua, Shen Tianyi, Zhu Nengjie, 2023. Triassic Compressional-Extensional Transition in Mengshan Area, NW Jiangxi Province, and Its Ore-Controlling Significance for Wollastonite Deposit. Earth Science, 48(11): 4053-4071. doi: 10.3799/dqkx.2022.500

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Triassic Compressional-Extensional Transition in Mengshan Area, NW Jiangxi Province, and Its Ore-Controlling Significance for Wollastonite Deposit

doi: 10.3799/dqkx.2022.500

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Administration of Geological Exploration of Jiangxi Province, Nanchang 330025, China
3.
No.224 Geological Brigade, Coal Geological Bureau of Jiangxi Province, Fenyi 330002, China

Received Date: 2022-11-13
Available Online: 2023-11-30
Publish Date: 2023-11-25

Abstract

Abstract

Mengshan, located in the middle of the western Pingxiang-Leping depression zone, have experienced complex tectono-magmatic processes during the Triassic, forming the Shizhushan giant wollastonite deposit. In order to reveal the structural ore-controlling mechanism of wollastonite deposit, in this study it probes into the rock deformation characteristics of different periods in detail based on the structural analysis of macroscopic and microscopic structural and the electron backscatter diffraction (EBSD) analysis of calcite. The results show that Mengshan experienced two tectonic deformation events during Triassic, indicating a tectonic regime transition from compression to extension. The D₁ event is characterized by low angle ductile thrust with top-to-the-SE, accompanied by intense calci-mylonitization. The D₂ event is a top-to-the-SSW extensional detachment related to the intrusion of the Mengshan granite. The deformed limestone is marmarosis and wollastonite mineralization. The microstructure analysis shows that the grain size and shape preferred orientation of calcite in the two deformed stages have different characteristics. EBSD results show that the D₁ deformed calcite displays a wide c-axis maximum close to Z, indicating monoclinic symmetry and a top-to-the-SE thrust shearing. The calcite of D₂ event developed randomly oriented c-axis poles, and underwent syn-tectonic recrystallization which resulted in resetting the microstructures of D₁ event. The Late Triassic Mengshan granite intruded into the first deformation zone as a post-kinematic product in an extensional tectonic background that provides time constraints for the deformations. The D₂ ductile detachment and wollastonite mineralization were both controlled by the extensional tectono-thermal system of the Mengshan granite. The extensional detachment leads to layered rich mineralization. The D₁ deformation can be related to the strong NW-SE compression widely developed in the Northwest Jiangxi Province, which was controlled by the collision of the South China block and North China block during the Middle Triassic. The D₂ deformation is the result of lithospheric extension adjustment in the Late Triassic on the basis of previous compressional deformation.
- Mengshan in Northwest Jiangxi,
- Triassic,
- compressional-extensional transition,
- ore-controlling structure,
- wollastonite mineralization,
- geodynamics,
- tectonics

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References(104)

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