准东构造隆升对砂岩型铀成矿作用的制约:磷灰石裂变径迹证据

宋继叶; 秦明宽; 蔡煜琦; 郭强; 何中波; 刘章月; 曹煦; 陈志国

doi:10.3799/dqkx.2018.331

Volume 44 Issue 11

Nov. 2019

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Article Navigation > Earth Science > 2019 > 44(11): 3910-3925

Song Jiye, Qin Mingkuan, Cai Yuqi, Guo Qiang, He Zhongbo, Liu Zhangyue, Cao Xu, Chen Zhiguo, 2019. Uplift-Denudation of Orogenic Belts Control on the Formation of Sandstone Type Uranium (U) Deposits in Eastern Junggar, Northwest China: Implications from Apatite Fission Track (AFT). Earth Science, 44(11): 3910-3925. doi: 10.3799/dqkx.2018.331

Citation:

Song Jiye, Qin Mingkuan, Cai Yuqi, Guo Qiang, He Zhongbo, Liu Zhangyue, Cao Xu, Chen Zhiguo, 2019. Uplift-Denudation of Orogenic Belts Control on the Formation of Sandstone Type Uranium (U) Deposits in Eastern Junggar, Northwest China: Implications from Apatite Fission Track (AFT). Earth Science, 44(11): 3910-3925. doi: 10.3799/dqkx.2018.331

Citation:

Song Jiye, Qin Mingkuan, Cai Yuqi, Guo Qiang, He Zhongbo, Liu Zhangyue, Cao Xu, Chen Zhiguo, 2019. Uplift-Denudation of Orogenic Belts Control on the Formation of Sandstone Type Uranium (U) Deposits in Eastern Junggar, Northwest China: Implications from Apatite Fission Track (AFT). Earth Science, 44(11): 3910-3925. doi: 10.3799/dqkx.2018.331

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Uplift-Denudation of Orogenic Belts Control on the Formation of Sandstone Type Uranium (U) Deposits in Eastern Junggar, Northwest China: Implications from Apatite Fission Track (AFT)

doi: 10.3799/dqkx.2018.331

Song Jiye^{1,2
,
,},
Qin Mingkuan^1,2,
Cai Yuqi^1,2,
Guo Qiang^1,2,
He Zhongbo^1,2,
Liu Zhangyue^1,2,
Cao Xu³,
Chen Zhiguo⁴

1.
Beijing Research Institute of Uranium Geology, Beijing 100029, China
2.
Key Laboratory of Uranium Resources Prospection and Evaluation Technology, CNNC, Beijing 100029, China
3.
China University of Geosciences, Beijing 100083, China
4.
Tianjin North China Geological Exploration Bureau, Tianjin 300170, China

Received Date: 2018-09-09
Publish Date: 2019-11-15

Abstract

Abstract

Apatite fission track dating and thermal history modeling were carried out on 12 granite samples collected from Kalamaili and Aokeshi Mountain in Eastern Junngar to investigate the uplift-denudation processes and characteristics of mountains, and then to discuss its control on sandstone U mineralization. Analyses results reveal the tectonic differential uplift-denudation of Kalamaili and Aokeshi Mountain, with Kalamaili area having been uplifting and being eroded since Late Triassic, much earlier than Aokeshi Mountain with uplifting in Late Jurassic, which plays an essential role in sandstone type U mineralization, including U source condition, the formation of tectonic-slope, favorable metallogenic structure and stable groundwater dynamics. The sandstone type U mineralization is different between the areas of Wucaiwan-Laojunmiao-Jiangjunmiao and Kamusite due to the differential uplift-denudation of the mountains under the tectonic background of transition from Indosinian to Yanshanian periods. Generally speaking, the conditions were better in Wucaiwan-Jiangjunmiao area in Early-Middle Jurassic while the conditions were better in the latter in Late Jurassic. Our study is a kind of sandstone type U mineralization which is going to provide the basic geology criteria for U resource prognosis.
- apatite fission track,
- tectonic uplift-denudation,
- mineralization condition of sandstone type U deposit,
- Eastern Junngar,
- tectonics

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Uplift-Denudation of Orogenic Belts Control on the Formation of Sandstone Type Uranium (U) Deposits in Eastern Junggar, Northwest China: Implications from Apatite Fission Track (AFT)

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