库车盆地早始新世成盐期卤水温度及其意义

徐洋; 曹养同; 刘成林

doi:10.3799/dqkx.2021.026

Volume 46 Issue 11

Nov. 2021

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Xu Yang, Cao Yangtong, Liu Chenglin, 2021. Brine Temperature of Early Eocene Salt Formation Period in Kuqa Basin and Its Significance. Earth Science, 46(11): 4188-4196. doi: 10.3799/dqkx.2021.026

Citation:

Xu Yang, Cao Yangtong, Liu Chenglin, 2021. Brine Temperature of Early Eocene Salt Formation Period in Kuqa Basin and Its Significance. Earth Science, 46(11): 4188-4196. doi: 10.3799/dqkx.2021.026

Xu Yang, Cao Yangtong, Liu Chenglin, 2021. Brine Temperature of Early Eocene Salt Formation Period in Kuqa Basin and Its Significance. Earth Science, 46(11): 4188-4196. doi: 10.3799/dqkx.2021.026

Citation:

Xu Yang, Cao Yangtong, Liu Chenglin, 2021. Brine Temperature of Early Eocene Salt Formation Period in Kuqa Basin and Its Significance. Earth Science, 46(11): 4188-4196. doi: 10.3799/dqkx.2021.026

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Brine Temperature of Early Eocene Salt Formation Period in Kuqa Basin and Its Significance

doi: 10.3799/dqkx.2021.026

Xu Yang^{1
,
,},
Cao Yangtong²,
Liu Chenglin^{2
,
,
,}

1.
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
2.
MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2021-02-07
Available Online: 2021-12-04
Publish Date: 2021-11-30

Abstract

Abstract

Paleoclimate and paleobrine temperature conditions are closely related to potassium formation in salt lakes. Quantitatively reconstructing evolution characteristics of paleobrine temperature during Early Eocene salt-forming period of the Kuqa basin has important scientific significance for evaluating the potash potential of the basin. In this paper it takes Lower Eocene rock salt of core QL1 which is located in the western Kuqa basin as research object for the first time. Based on the detailed petrographic research, the test and analysis of homogenization temperature of primary fluid inclusions of halite were carried out. The analysis results show that a total of 135 homogenization temperature data were obtained from six samples with different depths of the borehole, ranging from 21.2 to 57.8℃, with an average value of 31.8℃, the profile shows a slight warming trend from bottom to top in the vertical direction. The characteristics of homogenization temperature range, average homogenization temperature, and maximum homogenization temperature measured in this paper are consistent with the temperature data of the Tethys seawater in the same period, which further indicates reliability and rationality of homogenization temperature data. In addition, the high temperature condition is conducive to strong evaporation and concentration of water bodies, which is in good agreement with the thick evaporite series and potassium minerals deposited in the Early Eocene of the Kuqa basin.
- brine temperature,
- halite fluid inclusion,
- Early Eocene,
- Kuqa basin,
- Tethys realm,
- environmental geology

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References(54)

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Brine Temperature of Early Eocene Salt Formation Period in Kuqa Basin and Its Significance

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