地质温度计在桂东南那卜韧性剪切带花岗质糜棱岩中的适用性

辛良伟; 李赛赛; 冯佐海; 刘兴源; 吴江波; 王秋宇

doi:10.3799/dqkx.2022.382

Volume 49 Issue 6

Jun. 2024

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Article Navigation > Earth Science > 2024 > 49(6): 1946-1965

Xin Liangwei, Li Saisai, Feng Zuohai, Liu Xingyuan, Wu Jiangbo, Wang Qiuyu, 2024. Applicability of Geothermometer to Granitic Mylonites in Nabu Ductile Shear Zone, Southeast Guangxi. Earth Science, 49(6): 1946-1965. doi: 10.3799/dqkx.2022.382

Citation:

Xin Liangwei, Li Saisai, Feng Zuohai, Liu Xingyuan, Wu Jiangbo, Wang Qiuyu, 2024. Applicability of Geothermometer to Granitic Mylonites in Nabu Ductile Shear Zone, Southeast Guangxi. Earth Science, 49(6): 1946-1965. doi: 10.3799/dqkx.2022.382

Citation:

Xin Liangwei, Li Saisai, Feng Zuohai, Liu Xingyuan, Wu Jiangbo, Wang Qiuyu, 2024. Applicability of Geothermometer to Granitic Mylonites in Nabu Ductile Shear Zone, Southeast Guangxi. Earth Science, 49(6): 1946-1965. doi: 10.3799/dqkx.2022.382

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Applicability of Geothermometer to Granitic Mylonites in Nabu Ductile Shear Zone, Southeast Guangxi

doi: 10.3799/dqkx.2022.382

Xin Liangwei^{1, 2
,
,},
Li Saisai^{1, 2
,
,},
Feng Zuohai^{1, 2},
Liu Xingyuan^{1, 2},
Wu Jiangbo^{1, 2},
Wang Qiuyu^{1, 2}

1.
Collaborative Innovation Center for Exploration of Nonferrous Metal Deposits and Efficient Utilization of Resources by the Province and Ministry, Guilin University of Technology, Guilin 541004, China
2.
College of Earth Sciences, Guilin University of Technology, Guilin 541004, China

Received Date: 2022-08-30
Available Online: 2024-07-11
Publish Date: 2024-06-25

Abstract

Abstract

The measurement of metamorphic and deformation temperature of mylonites is of great significance for the interpretation of deformation evolution process and thermochronological isotope dating results. In this paper it only discusses the applicability of each geothermometers in the Nabu ductile shear zone. Using the plastic deformation characteristics, such as the mineral assemblage, dynamic recrystallization characteristics of minerals and EBSD (electron back-scattered diffraction) quartz c-axis fabrics in mylonites, the metamorphic deformation temperature range of the Nabu ductile shear zone is estimated to be 400 to 550 ℃. Based on the electron probe microanalysis (EMPA), the chlorite compositional geothermometer, muscovite-chlorite geothermometer, Ti-in-muscovite and Ti-in-biotite geothermometers were applied to calculate the metamorphic deformation temperature of the granitic mylonite samples in the Nabu ductile shear zone. The corresponding temperatures are 305 to 325 ℃, 390 to 500 ℃, 395 to 492 ℃ and 473 to 565 ℃, 431 to 574 ℃. Through comparative analysis, it is found that the results obtained by using chlorite compositional geothermometer are obviously lower than the temperature range estimated by using plastic deformation characteristics and the results calculated by other geothermometers. Combined with the results of previous studies, the chlorite compositional geothermometer is only suitable for the temperature calculation of low temperature metamorphic deformation. The results obtained by the other three geothermometers are all within the error range of the temperature estimated by using the plastic deformation characteristics, indicating that they are suitable for the calculation of metamorphic deformation temperature of the Nabu ductile shear zone. Among them, the muscovite-chlorite geothermometer is suitable for low temperature mylonite, and Ti-in-muscovite and Ti-in-biotite geothermometers are suitable for relatively high temperature mylonite.
- mylonitization,
- ductile shear zone,
- geothermometer,
- metamorphic deformation temperature,
- Nabu Town,
- tectonics

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致谢: 在电子探针和EBSD石英组构特征分析实验中，得到了桂林理工大学谢兰芳、刘奕志以及吴杰老师的大力支持，在此表示最诚挚的感谢！最后对两位匿名审稿专家对本文提出的建设性意见和责任编辑严谨的审阅表示衷心的感谢！

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Applicability of Geothermometer to Granitic Mylonites in Nabu Ductile Shear Zone, Southeast Guangxi

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