华北克拉通孔兹岩带磴口和佘太地区花岗片麻岩和斜长角闪岩变质锆石对其北界位置的再约束

段瑞涵; 刘超辉; 施建荣

doi:10.3799/dqkx.2020.080

Volume 45 Issue 9

Sep. 2020

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Article Navigation > Earth Science > 2020 > 45(9): 3386-3402

Duan Ruihan, Liu Chaohui, Shi Jianrong, 2020. Studies on Metamorphic Zircons of Granitic Gneisses and Amphibolites in the Dengkou and Shetai Areas of the Khondalite Belt of the North China Craton: More Constraints on Its Northern Boundary. Earth Science, 45(9): 3386-3402. doi: 10.3799/dqkx.2020.080

Citation:

Duan Ruihan, Liu Chaohui, Shi Jianrong, 2020. Studies on Metamorphic Zircons of Granitic Gneisses and Amphibolites in the Dengkou and Shetai Areas of the Khondalite Belt of the North China Craton: More Constraints on Its Northern Boundary. Earth Science, 45(9): 3386-3402. doi: 10.3799/dqkx.2020.080

Citation:

Duan Ruihan, Liu Chaohui, Shi Jianrong, 2020. Studies on Metamorphic Zircons of Granitic Gneisses and Amphibolites in the Dengkou and Shetai Areas of the Khondalite Belt of the North China Craton: More Constraints on Its Northern Boundary. Earth Science, 45(9): 3386-3402. doi: 10.3799/dqkx.2020.080

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Studies on Metamorphic Zircons of Granitic Gneisses and Amphibolites in the Dengkou and Shetai Areas of the Khondalite Belt of the North China Craton: More Constraints on Its Northern Boundary

doi: 10.3799/dqkx.2020.080

Duan Ruihan^{1
,
,},
Liu Chaohui^{1
,
,},
Shi Jianrong²

1.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
Tianjin Center, China Geological Survey, Tianjin 300170, China

Received Date: 2020-03-10
Publish Date: 2020-09-15

Abstract

Abstract

This paper presents a study of the mineral inclusions, U-Pb isotopes and trace elements of the metamorphic zircons from the granitic gneisses in the Dengkou area and the amphibolites in the Shetai area. The results show that the U-Pb age of one granite gneiss magmatic zircon in Dengkou area is 2 549±14 Ma, the age of metamorphic zircon is 1 874 ±26 Ma, and that of another granite gneiss metamorphic zircon is 1 877 ±25 Ma, and their REE patterns are generally left-leaning. On the other hand, the metamorphic zircons of the amphibolites in the Shetai area yield U-Pb ages of 1 924±25 Ma and 1 800±20 Ma in the south and 2 469±15 Ma in the north, respectively and they also show left-leaning REE patterns. Based on the rock assemblage, spatial distribution of the late Neoarchean and Paleoproterozoic metamorphic events, and the previous research results, we suggest that the north boundary of the Khondalite Belt in the Dengkou area more likely extends to the west, rather than the southwest as previously thought and the boundary in the Shetai area is distributed along the Wuchuan-Guyang-Shetai instead of along the Wuchuan-Guyang-Urad Houqi.
- North China Craton,
- Khondalite Belt,
- Paleoproterozoic,
- zircon U-Pb dating,
- trace elements,
- zircon mineral inclusion,
- petrology

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References(79)

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