尼日利亚中部纳萨拉瓦地区卡马伟晶岩型锂铌钽矿床锆石与锡石U-Pb年代学、Hf同位素组成及其地质意义

曹亮; 胡鹏; 姜军胜; 陈鑫; 向鹏; 李乐广; 卢山松; 赵凯; 童喜润; 王建青

doi:10.3799/dqkx.2024.116

Volume 49 Issue 11

Nov. 2024

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Article Navigation > Earth Science > 2024 > 49(11): 3971-3994

Cao Liang, Hu Peng, Jiang Junsheng, Chen Xin, Xiang Peng, Li Leguang, Lu Shansong, Zhao Kai, Tong Xirun, Wang Jianqing, 2024. Zircon and Cassiterite U-Pb Geochronology and Hf Isotopes of Kama Li-Nb-Ta Pegmatite Deposit and Its Geological Significance in Nasarawa, Central Nigeria. Earth Science, 49(11): 3971-3994. doi: 10.3799/dqkx.2024.116

Citation:

Cao Liang, Hu Peng, Jiang Junsheng, Chen Xin, Xiang Peng, Li Leguang, Lu Shansong, Zhao Kai, Tong Xirun, Wang Jianqing, 2024. Zircon and Cassiterite U-Pb Geochronology and Hf Isotopes of Kama Li-Nb-Ta Pegmatite Deposit and Its Geological Significance in Nasarawa, Central Nigeria. Earth Science, 49(11): 3971-3994. doi: 10.3799/dqkx.2024.116

Citation:

Cao Liang, Hu Peng, Jiang Junsheng, Chen Xin, Xiang Peng, Li Leguang, Lu Shansong, Zhao Kai, Tong Xirun, Wang Jianqing, 2024. Zircon and Cassiterite U-Pb Geochronology and Hf Isotopes of Kama Li-Nb-Ta Pegmatite Deposit and Its Geological Significance in Nasarawa, Central Nigeria. Earth Science, 49(11): 3971-3994. doi: 10.3799/dqkx.2024.116

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Zircon and Cassiterite U-Pb Geochronology and Hf Isotopes of Kama Li-Nb-Ta Pegmatite Deposit and Its Geological Significance in Nasarawa, Central Nigeria

doi: 10.3799/dqkx.2024.116

Cao Liang^{1, 2, 3
,
,},
Hu Peng^{1, 2
,
,
,},
Jiang Junsheng^{1, 2},
Chen Xin^{3, 4},
Xiang Peng^{1, 2},
Li Leguang⁵,
Lu Shansong¹,
Zhao Kai^{1, 2},
Tong Xirun¹,
Wang Jianqing⁶

1.
Wuhan Center, China Geological Survey (Central South China Innovation Center for Geosciences), Wuhan 430205, China
2.
Research Center for Petrogenesis and Mineralization of Granitoid Rocks, China Geological Survey, Wuhan 430205, China
3.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
4.
State Key Laboratory of Geological Processes and Mineral Resources, Wuhan 430074, China
5.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
6.
Tianjin North China Geological Exploration General Institute Co., Ltd, Tianjin 300170, China

Received Date: 2024-11-06
Publish Date: 2024-11-25

Abstract

Abstract

The Nasarawa region in central Nigeria is a typical area with developed lithium-niobium-tantalum rare metal pegmatite veins. The Kama granitic pegmatite-type rare metal deposit, located in the central part of the Nigerian lithium-niobium-tantalum-tin polymetallic metallogenic belt, is a newly discovered large deposit mainly containing lithium with associated niobium and tantalum ores. To define its metallogenic age and explore the sources and evolution of its mineralization process, this paper conducts a study of petrology, mineralogy, zircon and cassiterite U-Pb geochronology, zircon trace elements, and Lu-Hf isotopes on the ore-bearing pegmatite veins The zircon U-Pb dating yields the ages of (577.3±2.5) Ma (n=18, MSWD=6.4), and the cassiterite U-Pb dating yields the ages of (582.6±8.6) Ma (n=25, MSWD=0.72), therefore the pegmatite of the Kama deposit is inferred to have formed between 577 and 583 Ma, with the main mineralization occurring in the late Neoproterozoic. Trace elementsgeochemical analyses indicate that the pegmatites in the study area were formed during subduction-collision processes, with their magma source primarily being metamorphic sedimentary rocks, originating from the continental crust. The magma evolution process may have involved fractional crystallization of minerals such as plagioclase, apatite, and zircon. The intense fractional crystallization evolution of the magma results in rocks with highly differentiated evolutionary characteristics. The Hf isotopic compositions of zircon, cassiterite and columbite-tantalite in pegmatite show that the ε_Hf(t) value of zircon is between -20.6 and -19.0, and the T_DM2 value is 2.7 Ga; The ε_Hf(t) value of cassiterite is between -17.7 and -14.9, and the T_DM2 value varies between 2.4 Ga and 2.6 Ga. The ε_Hf(t) value of Columbite-tantalite is between -15.9 and -7.4, and the T_DM2 values are between 2.0 Ga and 2.4 Ga, indicating that the parent melt of pegmatite mainly originated from the remelting of Neoarchean-Proterozoic basement rocks. The mineralization of rare metal pegmatite deposits in Nigeria is closely related to Gondwana orogeny, which corresponds to the post-collision extension period of Gondwana orogeny.
- zircon U-Pb dating,
- cassiterite U-Pb dating,
- Hf,
- isotopes,
- trace elements,
- pegmatite,
- metallogenic age,
- Nigeria,
- geochemistry

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References(70)

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