大别山南缘翁门杂岩中太古代‒古元古代岩浆构造热事件的识别及其地质意义

徐大良; 彭练红; 邓新; 徐扬; 刘浩

doi:10.3799/dqkx.2023.042

Volume 48 Issue 11

Nov. 2023

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Article Navigation > Earth Science > 2023 > 48(11): 4072-4087

Xu Daliang, Peng Lianhong, Deng Xin, Xu Yang, Liu Hao, 2023. Identification of Mesoarchean to Paleoproterozoic Magmatic Tectono-Thermal Events from Wengmen Complex in Southern Dabie Orogen and Its Geological Significance. Earth Science, 48(11): 4072-4087. doi: 10.3799/dqkx.2023.042

Citation:

Xu Daliang, Peng Lianhong, Deng Xin, Xu Yang, Liu Hao, 2023. Identification of Mesoarchean to Paleoproterozoic Magmatic Tectono-Thermal Events from Wengmen Complex in Southern Dabie Orogen and Its Geological Significance. Earth Science, 48(11): 4072-4087. doi: 10.3799/dqkx.2023.042

Citation:

Xu Daliang, Peng Lianhong, Deng Xin, Xu Yang, Liu Hao, 2023. Identification of Mesoarchean to Paleoproterozoic Magmatic Tectono-Thermal Events from Wengmen Complex in Southern Dabie Orogen and Its Geological Significance. Earth Science, 48(11): 4072-4087. doi: 10.3799/dqkx.2023.042

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Identification of Mesoarchean to Paleoproterozoic Magmatic Tectono-Thermal Events from Wengmen Complex in Southern Dabie Orogen and Its Geological Significance

doi: 10.3799/dqkx.2023.042

Xu Daliang^{1, 2
,
,},
Peng Lianhong^{1
,
,},
Deng Xin^{1, 2},
Xu Yang^{1, 2},
Liu Hao¹

1.
Wuhan Center of China Geological Survey (China 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

Received Date: 2022-11-21
Available Online: 2023-11-30
Publish Date: 2023-11-25

Abstract

Abstract

The Wengmen complex, a newly identified Early Precambrian metamorphic basement with shallow metamorphism, opens a fresh avenue for future research on the formation and evolution of the early continental crust of the Dabie orogen on the northern Yangtze Block. In this paper, it presents a comprehensive study of in situ zircon U-Pb geochronology and Hf isotopes of representative meta-granitic rocks from the Wengmen complex. The results show that two meta-tonalite gneisses were formed at 2 914±24.5 Ma and 2 874±6.6 Ma respectively, two monzonitic granitic gneisses were formed at 2 669±10.7 Ma and 2 644±7.1 Ma respectively, and one mylonitized monzonitic granite was formed at 2 454±6.5 Ma, which confirms the existence of Archean to Early Paleoproterozoic continental crust basement in the southern Dabie orogen. The dating results also show that the formation ages of the two eyeball-like granitic gneisses are 2 011±6.3 Ma and 2 010±5.4 Ma, respectively. Moreover, ca. 2.0 Ga metamorphic zircon age has been obtained from the Wengmen Archean rocks, indicating that the complex may have been involved in the Paleoproterozoic orogenic event. The available data indicate that the newly discovered Wengmen complex in the southern Dabie orogen and the Kongling complex in the Yangtze continental core have synchronous tectono-magmatic thermal events and crustal accretion history during the Archean to Early Paleoproterozoic. However, the periphery of the Dabie orogen shows uniqueness due to its well-developed ~2.5 Ga tectono-magmatic thermal event, which is consistent with those of the ancient continental blocks in the world and may be the record of the final maturation and stabilization during the end of the Archean. Integrating the new and published data, it proposes that each basement on the northern Yangtze Block maybe coexisted in different parts of the Sclavia supercraton at the end of the Neoarchean, and the periphery of the Dabie orogen represented by the Wengmen complex maybe was located closer to the margin of the supercraton.
- Dabie orogen,
- metamorphic complex,
- Archean,
- Paleoproterozoic,
- zircon,
- crustal growth and reworking,
- supercraton,
- tectonics

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References(52)

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Identification of Mesoarchean to Paleoproterozoic Magmatic Tectono-Thermal Events from Wengmen Complex in Southern Dabie Orogen and Its Geological Significance

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