内蒙古巴尔哲稀有稀土矿区新发现的碱性流纹岩岩石成因及其地质意义

淡凯波; 张道涵; 栾钰薇; 宋崇宇; 于淼; 刘常伟

doi:10.3799/dqkx.2023.177

Volume 49 Issue 4

Apr. 2024

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Dan Kaibo, Zhang Daohan, Luan Yuwei, Song Chongyu, Yu Miao, Liu Changwei, 2024. Petrogenesis and Geological Significance of Newly Discovered Alkaline Rhyolite in Baerzhe Rare Metal Deposit, Inner Mongolia. Earth Science, 49(4): 1324-1338. doi: 10.3799/dqkx.2023.177

Citation:

Dan Kaibo, Zhang Daohan, Luan Yuwei, Song Chongyu, Yu Miao, Liu Changwei, 2024. Petrogenesis and Geological Significance of Newly Discovered Alkaline Rhyolite in Baerzhe Rare Metal Deposit, Inner Mongolia. Earth Science, 49(4): 1324-1338. doi: 10.3799/dqkx.2023.177

Citation:

Dan Kaibo, Zhang Daohan, Luan Yuwei, Song Chongyu, Yu Miao, Liu Changwei, 2024. Petrogenesis and Geological Significance of Newly Discovered Alkaline Rhyolite in Baerzhe Rare Metal Deposit, Inner Mongolia. Earth Science, 49(4): 1324-1338. doi: 10.3799/dqkx.2023.177

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Petrogenesis and Geological Significance of Newly Discovered Alkaline Rhyolite in Baerzhe Rare Metal Deposit, Inner Mongolia

doi: 10.3799/dqkx.2023.177

Dan Kaibo^{1
,
,},
Zhang Daohan^{2, 3
,
,},
Luan Yuwei²,
Song Chongyu^{2, 4},
Yu Miao⁵,
Liu Changwei⁶

1.
Luoyang Luanchuan Molybdenum Industry Group Co., Ltd., Luanchuan 471000, China
2.
School of Earth Resources, China University of Geosciences, China University of Geosciences, Wuhan 430074, China
3.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
4.
China Geological Survey Development Research Center, Beijing 100037, China
5.
Beijing Institute of Geological Hazard Prevention, Beijing 100120, China
6.
The Inner Mongolia Chifeng Geological Mineral Exploration and Development Co., Ltd., Chifeng 024005, China

Received Date: 2023-04-05
Available Online: 2024-04-30
Publish Date: 2024-04-25

Abstract

Abstract

To decipher the petrogenesis of the newly discovered alkaline rhyolite in the Baerzhe giant rare metal deposit in Inner Mongolia, and its genetic relationship with the ore⁃related peralkaline granite and Aliwula alkaline rhyolite from the adjacent area, in this research it carried out high spatial resolution LA-SF-ICP-MS zircon U-Pb dating, mineralogical and whole⁃rock geochemical studies. The results show that the eruption age of the Baerzhe alkaline rhyolite is 124.4±1.6 Ma, which is obviously younger than that of the Aliwula alkaline rhyolite(141 Ma), which represents a new stage of alkaline volcanic activity in the middle-southern section of the Great Xing'an Range during the Early Cretaceous. The Baerzhe and Aliwula alkaline rhyolites have high SiO₂, alkali metals, TFe₂O₃, F and low Al₂O₃ contents, and belong to comendites. Both are rich in light rare earth elements (LREE) and high field strength elements (HFSE) such as Nb, Ta, Zr, and Hf, and contain high Rb, Th, U and extremely low Ba and Sr contents. In addition, both have the same whole-rock Nd isotopic composition, with ε_Nd(t) values of 1.6 and 1.7-1.8, respectively. Therefore, both Baerzhe and Aliwula alkaline rhyolites are the products of partial melting of the juvenile lower crust. The Baerzhe alkaline rhyolite and ore⁃related peralkaline granite have the same formation age and isotope composition, and are different products of same, evolving magmatic system. Given the wider exposure range of volcanic rocks, alkaline volcanic rocks can be used as an important geological prospecting indicator for the underlying rare metal deposits, and it is pointed out that Aliwula area has a good prospecting potential for such deposits.
- Baerzhe,
- Aliwula,
- rare metal deposit,
- alkaline volcanic rock,
- Great Xing'an Range,
- ore deposit geology

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References(75)

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Petrogenesis and Geological Significance of Newly Discovered Alkaline Rhyolite in Baerzhe Rare Metal Deposit, Inner Mongolia

doi: 10.3799/dqkx.2023.177

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通讯作者: 陈斌, bchen63@163.com

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