盆山耦合机制驱动下的库车坳陷铀成矿作用响应

吴立群; 焦养泉; 王国荣; 王强强; 荣辉; 阿种明; 张帆; 鲁克改; 陶振鹏; 孙潇; 向尧

doi:10.3799/dqkx.2022.100

Volume 47 Issue 9

Sep. 2022

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Article Navigation > Earth Science > 2022 > 47(9): 3174-3191

Wu Liqun, Jiao Yangquan, Wang Guorong, Wang Qiangqiang, Rong Hui, A Zhongming, Zhang Fan, Lu Kegai, Tao Zhenpeng, Sun Xiao, Xiang Yao, 2022. Response of Uranium Mineralization in Kuqa Depression Driven by Basin⁃Mountain Coupling Mechanism. Earth Science, 47(9): 3174-3191. doi: 10.3799/dqkx.2022.100

Citation:

Wu Liqun, Jiao Yangquan, Wang Guorong, Wang Qiangqiang, Rong Hui, A Zhongming, Zhang Fan, Lu Kegai, Tao Zhenpeng, Sun Xiao, Xiang Yao, 2022. Response of Uranium Mineralization in Kuqa Depression Driven by Basin⁃Mountain Coupling Mechanism. Earth Science, 47(9): 3174-3191. doi: 10.3799/dqkx.2022.100

Citation:

Wu Liqun, Jiao Yangquan, Wang Guorong, Wang Qiangqiang, Rong Hui, A Zhongming, Zhang Fan, Lu Kegai, Tao Zhenpeng, Sun Xiao, Xiang Yao, 2022. Response of Uranium Mineralization in Kuqa Depression Driven by Basin⁃Mountain Coupling Mechanism. Earth Science, 47(9): 3174-3191. doi: 10.3799/dqkx.2022.100

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Response of Uranium Mineralization in Kuqa Depression Driven by Basin⁃Mountain Coupling Mechanism

doi: 10.3799/dqkx.2022.100

Wu Liqun^{1, 2
,
,},
Jiao Yangquan^{1, 2},
Wang Guorong³,
Wang Qiangqiang³,
Rong Hui^{1, 2},
A Zhongming³,
Zhang Fan^{1, 2},
Lu Kegai³,
Tao Zhenpeng⁴,
Sun Xiao³,
Xiang Yao^{1, 2}

1.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
Geologic Party No. 216, CNNC, Urumqi 830011, China
4.
School of Architectural Engineering, Huanggang Normal University, Huanggang 438000, China

Received Date: 2022-03-20
Publish Date: 2022-09-25

Abstract

Abstract

Uranium mineralization around Kuqa depression is very active. The ore-controlling factors, metallogenic mechanism and metallogenic law, especially the prospective selection, of sandstone⁃type uranium deposits in the lower member of Pliocene Kuqa Formation have become the focus of uranium geologists in recent years. Based on the regional geological data, field geological survey and exploration drilling data, through comprehensive analysis, the author attempts to analyze the key ore-controlling factors and spatial and temporal collocation relationship of the formation and development of sandstone⁃type uranium deposits in the context of basin⁃mountain coupling mechanism (tectonics & sediments & geomorphology), following the general metallogenic mechanism of sandstone⁃type uranium deposits and the research idea from source to sink. From the perspective of uranium metallogenic system analysis, the cooperative ore control mechanism of key ore⁃controlling elements of Kuqa Formation is revealed in order to provide strategic services for uranium exploration. It is found that large-scale intracontinental thrust nappe of the Cenozoic South Tianshan orogenic belt not only controls the filling evolution process of the uranium bearing rock series of the Kuqa Formation, but also restricts the basic pattern and metallogenic process of uranium mineralization in the lower member of the Kuqa Formation. The basin⁃mountain coupling mechanism is the original force driving the formation and development of sandstone⁃type uranium deposits. Although the distribution scale of magmatic rocks in the South Tianshan orogen is limited, U-rich granites exist in the Tomur peak area. The fully developed surface water drainage system, on the one hand, can carry the debris of the orogenic belt to accumulate in the Kuqa depression, thus forming a series of large provenance-sedimentary lobes in stages, creating potential uranium bearing rock series and high-quality uranium reservoir. On the other hand, the drainage system crossing the U-rich granites in the orogenic belt not only provides the accumulation of original trace uranium for the uranium reservoir through physical transportation, but also promotes the development of regional interlayer oxidation zone and dissolved uranium required for mineralization through the derived underground ore-bearing fluid system. In Kuqa depression, the near East-West structure limits the ore-bearing flow field and the development space of interlayer oxidation zone (Baicheng sag). Uranium mineralization is concentrated near the front line of regional interlayer oxidation zone (especially the "water blocking surface" side in the South).At the southern edge of Baicheng sag, with the continuous uplift of Qiulitage structural belt with synsedimentary growth property, the regional ore-bearing flow field and interlayer oxidation zone were forced to migrate northward and caused "left-lateral" movement, thus creating "new" and "old" uranium metallogenic systems including Ridarik uranium deposit.
- sandstone⁃type uranium deposit,
- ore⁃controlling factors,
- uranium metallogenic system,
- basin⁃mountain coupling,
- lower member of Kuqa Formation,
- Kuqa depression,
- mineral deposit

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References(94)

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