内蒙古合教BIF型铁矿的形成时代、地球化学特征及地质意义

王佳营; 李志丹; 李光耀; 文思博; 谢瑜; 张祺; 张锋; 丁宁

doi:10.3799/dqkx.2019.211

Volume 45 Issue 6

Jun. 2020

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Article Navigation > Earth Science > 2020 > 45(6): 2135-2151

Wang Jiaying, Li Zhidan, Li Guangyao, Wen Sibo, Xie Yu, Zhang Qi, Zhang Feng, Ding Ning, 2020. Formation Age, Geochemical Signatures and Geological Significance of the Hejiao Iron Deposit, Inner Mongolia. Earth Science, 45(6): 2135-2151. doi: 10.3799/dqkx.2019.211

Citation:

Wang Jiaying, Li Zhidan, Li Guangyao, Wen Sibo, Xie Yu, Zhang Qi, Zhang Feng, Ding Ning, 2020. Formation Age, Geochemical Signatures and Geological Significance of the Hejiao Iron Deposit, Inner Mongolia. Earth Science, 45(6): 2135-2151. doi: 10.3799/dqkx.2019.211

Citation:

Wang Jiaying, Li Zhidan, Li Guangyao, Wen Sibo, Xie Yu, Zhang Qi, Zhang Feng, Ding Ning, 2020. Formation Age, Geochemical Signatures and Geological Significance of the Hejiao Iron Deposit, Inner Mongolia. Earth Science, 45(6): 2135-2151. doi: 10.3799/dqkx.2019.211

PDF( 9551 KB)

Formation Age, Geochemical Signatures and Geological Significance of the Hejiao Iron Deposit, Inner Mongolia

doi: 10.3799/dqkx.2019.211

Wang Jiaying^{1, 2
,
,},
Li Zhidan^{1, 2
,
,
,},
Li Guangyao^{1, 2},
Wen Sibo^{1, 2},
Xie Yu^{1, 2},
Zhang Qi^{1, 2},
Zhang Feng^{1, 2},
Ding Ning³

1.
Tianjin Center, China Geological Survey, Tianjin 300170, China
2.
Key Laboratory of Uranium Geology, China Geological Survey, Tianjin 300170, China
3.
The First Monitoring and Application Center, China Earthquake Administration, Tianjin 300180, China

Received Date: 2019-05-22
Publish Date: 2020-06-15

Abstract

Abstract

The Hejiao iron deposit in Inner Mongolia, which is located in the Yinshan block on the northern margin of western block of the North China craton, is a medium-sized BIF-type iron deposit in the Guyang greenstone belt. Geochronology and petrogeochemistry of amphibolite and iron ore were studied in this paper. LA-ICP-MS U-Pb dating of zircons from the amphibolites interlayer shows that cores of the zircons characterized by core-rim texture and with a Th/U ratio of higher than 0.1(0.27-1.00) have an upper intercept age of 2 549±29 Ma(MSWD=0.51), which is approximately the depositional age of the Hejiao BIF-type iron deposit, during which widespread tectonic-tectonothermal event and most BIFs occurrence took place at the Early Cambrian of North China craton. A protolith reconstruction shows that the protolith of amphibolites is basalt, indicating that Hejiao iron deposit belongs to Algoma-type BIF closely related to volcanic activities. The chondrite-normalized REE pattern of amphibolites is nearly flat, similar to those of E-MORB and back-arc basin basalts (BABB). Primitive mantle-normalized trace element pattern of amphibolites is similar to back-arc basin basalts (BABB), showing enrichment in LILEs such as Rb, Ba, Sr, K, and depletion in HFSEs such as Nb, Ta, U, Th, similar to the characteristics of island arc magmatic rocks. Combining the model of island arc-mantle plume interaction for the Guyang greenstone belt, it is speculated that the amohibolites were formed in a tectonic setting of back-arc basin, accompanied by mantle plume, which implies the tectonic environment of the Hejiao BIF. The characteristics of the iron ores include the depletion of LREE, enrichment of HREE[(La/Yb)_PAAS=0.29-0.50], slightly positive La anomaly(La/La^*=1.00-1.13), strongly positive Eu anomaly (Eu/Eu^*=1.54-2.27), positive Y anomaly(Y/Y^*=1.07-1.42), and no distinct Ce anomalies(Ce/Ce^*=0.90-0.95).Based on the similar signatures to the komatiite at bottom of the Guyang greenstone belt and the mixture of high-temperature hydrothermal fluid and seawater, it is inferred that Fe of the Hejiao BIF-type iron deposit was supplied through the high-temperature hydrothermal leaching of komatiites.
- BIF-type iron deposit,
- U-Pb dating of zircons,
- geochemistry,
- North China craton,
- Hejiao

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References(88)

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Formation Age, Geochemical Signatures and Geological Significance of the Hejiao Iron Deposit, Inner Mongolia

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